CICE: (prism_init) calling prism_init_comp_proto... CICE: (prism_init) calling prism_init_comp_proto... CICE: (prism_init) calling prism_init_comp_proto... CICE: (prism_init) calling prism_init_comp_proto... CICE: (prism_init) calling prism_init_comp_proto... CICE: (prism_init) calling prism_init_comp_proto... CICE: (prism_init) calling prism_init_comp_proto... CICE: (prism_init) calling prism_init_comp_proto... CICE: (prism_init) calling prism_init_comp_proto... CICE: (prism_init) calling prism_init_comp_proto... CICE: (prism_init) calling prism_init_comp_proto... CICE: (prism_init) calling prism_init_comp_proto... CICE: (prism_init) calling prism_init_comp_proto... CICE: (prism_init) calling prism_init_comp_proto... CICE: (prism_init) calling prism_init_comp_proto... CICE: (prism_init) calling prism_init_comp_proto... CICE: (prism_init) calling prism_init_comp_proto... CICE: (prism_init) calling prism_init_comp_proto... CICE: (prism_init) calling prism_init_comp_proto... CICE: (prism_init) calling prism_init_comp_proto... CICE: (prism_init) calling prism_init_comp_proto... CICE: (prism_init) calling prism_init_comp_proto... CICE: (prism_init) calling prism_init_comp_proto... CICE: (prism_init) calling prism_init_comp_proto... MOCN: _get_localcomm_ OK! il_commlocal= 3 CICE: (prism_init) called prism_init_comp_proto ! CICE: (prism_init) MPI_Buffer_Attach ok! CICE: _get_localcomm_ OK! il_commlocal= 3 * CICE: Entering init_cpl..... * CICE4 (init_cpl) calling MPI_Comm_Size ... * CICE4 (init_cpl) calling MPI_Comm_Rank ... * CICE4 (init_cpl) il_commlocal, il_nbtotproc, my_task = 3 24 16 CICE: (prism_init) called prism_init_comp_proto ! CICE: (prism_init) MPI_Buffer_Attach ok! CICE: _get_localcomm_ OK! il_commlocal= 3 * CICE: Entering init_cpl..... * CICE4 (init_cpl) calling MPI_Comm_Size ... * CICE4 (init_cpl) calling MPI_Comm_Rank ... * CICE4 (init_cpl) il_commlocal, il_nbtotproc, my_task = 3 24 18 CICE: (prism_init) called prism_init_comp_proto ! CICE: (prism_init) MPI_Buffer_Attach ok! CICE: _get_localcomm_ OK! il_commlocal= 3 * CICE: Entering init_cpl..... * CICE4 (init_cpl) calling MPI_Comm_Size ... * CICE4 (init_cpl) calling MPI_Comm_Rank ... * CICE4 (init_cpl) il_commlocal, il_nbtotproc, my_task = 3 24 21 CICE: (prism_init) called prism_init_comp_proto ! CICE: (prism_init) MPI_Buffer_Attach ok! CICE: _get_localcomm_ OK! il_commlocal= 3 * CICE: Entering init_cpl..... * CICE4 (init_cpl) calling MPI_Comm_Size ... * CICE4 (init_cpl) calling MPI_Comm_Rank ... * CICE4 (init_cpl) il_commlocal, il_nbtotproc, my_task = 3 24 20 CICE: (prism_init) called prism_init_comp_proto ! CICE: (prism_init) MPI_Buffer_Attach ok! CICE: _get_localcomm_ OK! il_commlocal= 3 * CICE: Entering init_cpl..... * CICE4 (init_cpl) calling MPI_Comm_Size ... CICE: (prism_init) called prism_init_comp_proto ! CICE: (prism_init) MPI_Buffer_Attach ok! CICE: _get_localcomm_ OK! il_commlocal= 3 * CICE: Entering init_cpl..... CICE: (prism_init) called prism_init_comp_proto ! CICE: (prism_init) MPI_Buffer_Attach ok! CICE: _get_localcomm_ OK! il_commlocal= 3 * CICE: Entering init_cpl..... * CICE4 (init_cpl) calling MPI_Comm_Size ... * CICE4 (init_cpl) calling MPI_Comm_Rank ... * CICE4 (init_cpl) il_commlocal, il_nbtotproc, my_task = 3 24 5 * CICE4 (init_cpl) calling MPI_Comm_Size ... * CICE4 (init_cpl) calling MPI_Comm_Rank ... * CICE4 (init_cpl) il_commlocal, il_nbtotproc, my_task = 3 24 23 CICE: (prism_init) called prism_init_comp_proto ! CICE: (prism_init) MPI_Buffer_Attach ok! CICE: _get_localcomm_ OK! il_commlocal= 3 * CICE: Entering init_cpl..... * CICE4 (init_cpl) calling MPI_Comm_Size ... * CICE4 (init_cpl) calling MPI_Comm_Rank ... * CICE4 (init_cpl) il_commlocal, il_nbtotproc, my_task = 3 24 0 * CICE4 (init_cpl) calling MPI_Comm_Rank ... * CICE4 (init_cpl) il_commlocal, il_nbtotproc, my_task = 3 24 1 CICE: (prism_init) called prism_init_comp_proto ! CICE: (prism_init) MPI_Buffer_Attach ok! CICE: _get_localcomm_ OK! il_commlocal= 3 * CICE: Entering init_cpl..... * CICE4 (init_cpl) calling MPI_Comm_Size ... * CICE4 (init_cpl) calling MPI_Comm_Rank ... * CICE4 (init_cpl) il_commlocal, il_nbtotproc, my_task = 3 24 7 CICE: (prism_init) called prism_init_comp_proto ! CICE: (prism_init) MPI_Buffer_Attach ok! CICE: _get_localcomm_ OK! il_commlocal= 3 * CICE: Entering init_cpl..... * CICE4 (init_cpl) calling MPI_Comm_Size ... * CICE4 (init_cpl) calling MPI_Comm_Rank ... * CICE4 (init_cpl) il_commlocal, il_nbtotproc, my_task = 3 24 15 CICE: (prism_init) called prism_init_comp_proto ! CICE: (prism_init) MPI_Buffer_Attach ok! CICE: _get_localcomm_ OK! il_commlocal= 3 * CICE: Entering init_cpl..... * CICE4 (init_cpl) calling MPI_Comm_Size ... * CICE4 (init_cpl) calling MPI_Comm_Rank ... * CICE4 (init_cpl) il_commlocal, il_nbtotproc, my_task = 3 24 8 CICE: (prism_init) called prism_init_comp_proto ! CICE: (prism_init) MPI_Buffer_Attach ok! CICE: _get_localcomm_ OK! il_commlocal= 3 * CICE: Entering init_cpl..... * CICE4 (init_cpl) calling MPI_Comm_Size ... * CICE4 (init_cpl) calling MPI_Comm_Rank ... * CICE4 (init_cpl) il_commlocal, il_nbtotproc, my_task = 3 24 17 CICE: (prism_init) called prism_init_comp_proto ! CICE: (prism_init) MPI_Buffer_Attach ok! CICE: _get_localcomm_ OK! il_commlocal= 3 * CICE: Entering init_cpl..... * CICE4 (init_cpl) calling MPI_Comm_Size ... * CICE4 (init_cpl) calling MPI_Comm_Rank ... * CICE4 (init_cpl) il_commlocal, il_nbtotproc, my_task = 3 24 4 CICE: (prism_init) called prism_init_comp_proto ! CICE: (prism_init) MPI_Buffer_Attach ok! CICE: _get_localcomm_ OK! il_commlocal= 3 * CICE: Entering init_cpl..... * CICE4 (init_cpl) calling MPI_Comm_Size ... * CICE4 (init_cpl) calling MPI_Comm_Rank ... * CICE4 (init_cpl) il_commlocal, il_nbtotproc, my_task = 3 24 22 CICE: (prism_init) called prism_init_comp_proto ! CICE: (prism_init) MPI_Buffer_Attach ok! CICE: _get_localcomm_ OK! il_commlocal= 3 * CICE: Entering init_cpl..... * CICE4 (init_cpl) calling MPI_Comm_Size ... * CICE4 (init_cpl) calling MPI_Comm_Rank ... * CICE4 (init_cpl) il_commlocal, il_nbtotproc, my_task = 3 24 19 CICE: (prism_init) called prism_init_comp_proto ! CICE: (prism_init) MPI_Buffer_Attach ok! CICE: _get_localcomm_ OK! il_commlocal= 3 * CICE: Entering init_cpl..... * CICE4 (init_cpl) calling MPI_Comm_Size ... * CICE4 (init_cpl) calling MPI_Comm_Rank ... * CICE4 (init_cpl) il_commlocal, il_nbtotproc, my_task = 3 24 13 CICE: (prism_init) called prism_init_comp_proto ! CICE: (prism_init) MPI_Buffer_Attach ok! CICE: _get_localcomm_ OK! il_commlocal= 3 * CICE: Entering init_cpl..... * CICE4 (init_cpl) calling MPI_Comm_Size ... * CICE4 (init_cpl) calling MPI_Comm_Rank ... * CICE4 (init_cpl) il_commlocal, il_nbtotproc, my_task = 3 24 11 CICE: (prism_init) called prism_init_comp_proto ! CICE: (prism_init) MPI_Buffer_Attach ok! CICE: _get_localcomm_ OK! il_commlocal= 3 * CICE: Entering init_cpl..... * CICE4 (init_cpl) calling MPI_Comm_Size ... * CICE4 (init_cpl) calling MPI_Comm_Rank ... * CICE4 (init_cpl) il_commlocal, il_nbtotproc, my_task = 3 24 6 * CICE: prism_init called OK! CICE: (prism_init) called prism_init_comp_proto ! CICE: (prism_init) MPI_Buffer_Attach ok! CICE: _get_localcomm_ OK! il_commlocal= 3 * CICE: Entering init_cpl..... * CICE4 (init_cpl) calling MPI_Comm_Size ... * CICE4 (init_cpl) calling MPI_Comm_Rank ... * CICE4 (init_cpl) il_commlocal, il_nbtotproc, my_task = 3 24 9 * CICE: prism_init called OK! CICE: (prism_init) called prism_init_comp_proto ! CICE: (prism_init) MPI_Buffer_Attach ok! CICE: _get_localcomm_ OK! il_commlocal= 3 * CICE: Entering init_cpl..... * CICE4 (init_cpl) calling MPI_Comm_Size ... * CICE4 (init_cpl) calling MPI_Comm_Rank ... * CICE4 (init_cpl) il_commlocal, il_nbtotproc, my_task = 3 24 12 * CICE: prism_init called OK! CICE: (prism_init) called prism_init_comp_proto ! CICE: (prism_init) MPI_Buffer_Attach ok! CICE: _get_localcomm_ OK! il_commlocal= 3 * CICE: Entering init_cpl..... * CICE4 (init_cpl) calling MPI_Comm_Size ... * CICE4 (init_cpl) calling MPI_Comm_Rank ... * CICE4 (init_cpl) il_commlocal, il_nbtotproc, my_task = 3 24 10 * CICE: prism_init called OK! CICE: (prism_init) called prism_init_comp_proto ! CICE: (prism_init) MPI_Buffer_Attach ok! CICE: _get_localcomm_ OK! il_commlocal= 3 * CICE: Entering init_cpl..... * CICE4 (init_cpl) calling MPI_Comm_Size ... * CICE4 (init_cpl) calling MPI_Comm_Rank ... * CICE4 (init_cpl) il_commlocal, il_nbtotproc, my_task = 3 24 2 CICE: (prism_init) called prism_init_comp_proto ! CICE: (prism_init) MPI_Buffer_Attach ok! CICE: _get_localcomm_ OK! il_commlocal= 3 * CICE: Entering init_cpl..... * CICE4 (init_cpl) calling MPI_Comm_Size ... * CICE4 (init_cpl) calling MPI_Comm_Rank ... * CICE4 (init_cpl) il_commlocal, il_nbtotproc, my_task = 3 24 3 * CICE: prism_init called OK! CICE: (prism_init) called prism_init_comp_proto ! CICE: (prism_init) MPI_Buffer_Attach ok! CICE: _get_localcomm_ OK! il_commlocal= 3 * CICE: Entering init_cpl..... * CICE4 (init_cpl) calling MPI_Comm_Size ... * CICE4 (init_cpl) calling MPI_Comm_Rank ... * CICE4 (init_cpl) il_commlocal, il_nbtotproc, my_task = 3 24 14 * CICE: prism_init called OK! * CICE: prism_init called OK! * CICE: prism_init called OK! * CICE: prism_init called OK! * CICE: prism_init called OK! * CICE: prism_init called OK! * CICE: prism_init called OK! * CICE: prism_init called OK! * CICE: prism_init called OK! * CICE: prism_init called OK! * CICE: prism_init called OK! * CICE: prism_init called OK! * CICE: prism_init called OK! * CICE: prism_init called OK! * CICE: prism_init called OK! * CICE: prism_init called OK! * CICE: prism_init called OK! * CICE: prism_init called OK! * CICE: prism_init called OK! nf90_inquire_dimension: longitude 1440 nf90_inquire_dimension: latitude 720 nf90_inquire_dimension: time 365 Reading setup_nml NOTE from PE 0: MPP_DOMAINS_SET_STACK_SIZE: stack size set to 32768. &MPP_IO_NML HEADER_BUFFER_VAL = 16384, GLOBAL_FIELD_ON_ROOT_PE = T, IO_CLOCKS_ON = F, SHUFFLE = 0, DEFLATE_LEVEL = -1 / NOTE from PE 0: MPP_IO_SET_STACK_SIZE: stack size set to 131072. Reading grid_nml Reading tracer_nml Reading thermo_nml Reading dynamics_nml Reading shortwave_nml Reading ponds_nml Reading forcing_nml Diagnostic output will be in file ice_diag.d ======== MODEL BEING DRIVEN BY OCEAN_SOLO_MOD ======== &OCEAN_SOLO_NML DATE_INIT = 3*1, 3*0, CALENDAR = NOLEAP , YEARS = 5, MONTHS = 0, DAYS = 0, HOURS = 0, MINUTES = 0, SECONDS = 0, DT_CPLD = 3600, N_MASK = 0, LAYOUT_MASK = 2*0, MASK_LIST = 4096*0, RESTART_INTERVAL = 6*0 / Reading zbgc_nml NOTE from PE 0: diag_manager_mod::diag_manager_init: Out of Range warnings will be ignored. NOTE from PE 0: diag_manager_mod::diag_manager_init: prepend_date only supported when diag_manager_init is called with time_init present. &OCEAN_PARAMETERS_NML CP_OCEAN = 3992.10322329649 , CP_LIQUID_RUNOFF = 4218.00000000000 , CP_SOLID_RUNOFF = 2106.00000000000 , RHO0 = 1035.00000000000 , TFREEZE = 273.150000000000 , OMEGA_EARTH = 7.292100000000000E-005, GRAV = 9.80000000000000 / ======== STARTING MOM INITIALIZATION ======== ==>NOTE: Using dynamically allocated array option in MOM &OCEAN_MODEL_NML TIME_TENDENCY = twolevel , IMPOSE_INIT_FROM_RESTART = F, REINITIALIZE_THICKNESS = F, BAROCLINIC_SPLIT = 1, BAROTROPIC_SPLIT = 80, SURFACE_HEIGHT_SPLIT = 1, LAYOUT = 16, 15, IO_LAYOUT = 2*0, DEBUG = F, VERTICAL_COORDINATE = zstar , DT_OCEAN = 3600, CMIP_UNITS = T, HORIZONTAL_GRID = bgrid , USE_BLOBS = F, USE_VELOCITY_OVERRIDE = F, MASK_TABLE = INPUT/ocean_mask_table , INTRODUCE_BLOBS = F, BETA_TXTY = 0.000000000000000E+000, BETA_TF = 0.000000000000000E+000, BETA_QF = 0.000000000000000E+000, BETA_LWSW = 0.000000000000000E+000 / ==>Note: Running MOM using 240 computer processors. ==>Note: Running MOM with staggered twotime level scheme to compute time tenden cies. This is the default. Mass/volume and tracer are conserved with this sc heme. ==>Note: Time%Time_init = time stamp at very start of the MOM experiment is given by yyyy/mm/dd hh:mm:ss = 1/ 1/ 1 0: 0: 0 ==>Note: Time%model_time = time stamp at start of this leg of the MOM experiment is yyyy/mm/dd hh:mm:ss = 1/ 1/ 1 0: 0: 0 ==>Note: Time%init=.true. =>MOM will start from user specified initial conditions. ==> Note: time steps (seconds) used for MOM dtts (tracer) = 3600.00 dtuv (baroclinic) = 3600.00 dteta (surface height or bottom pressure) = 3600.00 dtbt (barotropic) = 45.00 ==> Note: The velocity equations will be split into baroclinic and barotropic pieces. ==> Note: Using MOM with B-grid horizontal layout of variables on a grid. ==> Note: Using MOM with zstar vertical coordinate. The equations are Boussinesq, and so conserve volume rather than mass. Use one of the pressure-like coordinates to get non-Boussinesq effects. &OCEAN_GRIDS_NML DEBUG_THIS_MODULE = T, VERBOSE_INIT = T, READ_RHO0_PROFILE = F, DO_BITWISE_EXACT_SUM = F, WRITE_GRID = F / ==>Note from ocean_grids_mod(set_ocean_grid_size): read grid from new version g rid NOTE from PE 0: ==>Note from ocean_grids_mod(set_ocean_grid_size): x_boundary_type is cyclic NOTE from PE 0: ==>Note from ocean_grids_mod(set_ocean_grid_size): y_boundary_type is fold_north_edge ==> Note: Energy conversion errors are nontrivial when using tripolar=.true. The cause is related to the need to update redundantly computed information across the Arctic bipolar fold in a bit-wise exact manner for terms contributing to the energy conversion analysis. The extra code and mpp calls have not been implemented. &OCEAN_DOMAINS_NML HALO = 1, MAX_TRACERS = 20, X_CYCLIC_OFFSET = 0, Y_CYCLIC_OFFSET = 0 / mom_domain domain decomposition whalo = 1, ehalo = 1, shalo = 1, nhalo = 1 X-AXIS = 23 23 23 23 22 22 22 22 22 22 22 22 23 23 23 23 Y-AXIS = 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 NOTE from PE 0: mpp_domains_define.inc(mpp_define_io_domain): io domain will not be defined for mom_domain when one or both entry of io_layout is not positive NOTE from PE 0: MPP_DOMAINS_SET_STACK_SIZE: stack size set to 1100000. NOTE from PE 0: ==>Note from ocean_grids_mod (set_ocean_hgrid_arrays): altering U-grid arrays at j=0 [chksum] xt -3425757943572301981 [chksum] xu -3428710751629949619 [chksum] yt 3983075590363002848 [chksum] yu 3993847596950837321 [chksum] dxt -2283612313907751155 [chksum] dxu -2282596789105961533 [chksum] dyt -2709740667792722851 [chksum] dyu -2692970264633898449 [chksum] dat -3833792397622233343 [chksum] dau -3813044238012496823 [chksum] dxtn -2282490927786808430 [chksum] dytn -2710847642103460454 [chksum] dxte -2283716151863231756 [chksum] dyte -2691860715696530614 [chksum] dxun -2281501901114313535 [chksum] dyun -2691323231969450374 [chksum] dxue -2282695913974554706 [chksum] dyue -2682318759084445648 [chksum] dtn+dts -2709740667792722851 [chksum] dun+dus -2692970264633898449 [chksum] dte+dtw -2283612313907751155 [chksum] due+duw -2282596789105961533 [chksum] dte -3364529801584597109 [chksum] dtw -3364422647368743287 [chksum] due -3363511944916596356 [chksum] duw -3363409454433164794 [chksum] sin_rot -426010600135597922 [chksum] cos_rot -1118842446256944817 &OCEAN_TOPOG_NML FLAT_BOTTOM = F, FLAT_BOTTOM_KMT = 50, FLAT_BOTTOM_HT = 5500.00000000000 , WRITE_TOPOG = F, MIN_THICKNESS = 25.0000000000000 , KMT_RECOMPUTE = F, KMT_RECOMPUTE_OFFSET = 0, DEBUG_THIS_MODULE = T / Topography checksums [chksum] ht -2435776769067813075 The shallowest wet ocean model grid cell has depth (meters) 45.11149 and this occurs at (i,j,k) = ( 40,288, 5) which has (long,lat,depth) = ( -260.7610, 76.8858, 45.11149) Beware that shallow regions (e.g., those shallower than 50m) may be subject to numerical problems if strong surface forcing is not mixed vertically. Such problems may occur especially in shallow regions with kmt==2. Current speeds and/or tracer deviations may become large due to the deposition of wind and/or buoyancy over just a small upper ocean region. Such problems can be resolved by adding sufficient vertical mixing in these regions. Such happens in Nature due to tides and breaking surface waves. [chksum] hu 6340078932675900470 [chksum] htr 972271619753254155 [chksum] kmu 5346 [chksum] kmt 5749 &OCEAN_OBC_NML NOBC = 0, DIRECTION = , NAME = test_obc none none none , IS = 4*-999, IE = 4*-999, JS = 4*-999, JE = 4*-999, IERS = 4*-999, IERE = 4*-999, JERS = 4*-999, JERE = 4*-999, ITRS = 4*-999, ITRE = 4*-999, JTRS = 4*-999, JTRE = 4*-999, OBC_NOR = NOGRAD NOGRAD NOGRAD NOGRAD , OBC_TAN = NOGRAD NOGRAD NOGRAD NOGRAD , OBC_ETA = NOTHIN NOTHIN NOTHIN NOTHIN , OBC_UD = NOGRAD NOGRAD NOGRAD NOGRAD , OBC_TRA = NOGRAD NOGRAD NOGRAD NOGRAD NOGRAD NOGRAD NOGRAD NOGRAD NOGRAD NOGRAD NOGRAD NOGRAD NOGRAD NOGRAD NOGRAD NO GRAD NOGRAD NOGRAD NOGRAD NOGRAD NOGRAD NOGRAD NOGRAD NOGRAD NOGRAD NOGRAD NOGRAD NOGRAD NOGRAD NOGRAD NOGRAD NOGRAD NOGRAD NOGRAD NOGRAD NOGRAD NOGRAD NOGRAD NOGRAD NOGRAD , OBC_MIX = NOGRAD NOGRAD NOGRAD NOGRAD , REL_COEF_ETA_IN = 4*0.000000000000000E+000 , REL_COEF_ETA_OUT = 4*0.000000000000000E+000 , REL_ETA_PNTS = 4*1, REL_CLIN_PNTS = 40*1, CTROP_MAX = 4*1.50000000000000 , CTROP_MIN = 4*0.100000000000000 , CTROP_INC = 4*0.000000000000000E+000 , CTROP_SMOOTH = 4*0.700000000000000 , FILENAME_ETA = obc_eta_t.nc none none none , FIELDNAME_ETA = eta_t none none none , FILENAME_UD = obc_ud.nc none none none , FIELDNAME_UD = ud none none none , OBC_CONSIDER_CONVU = 4*F, OBC_ADJUST_FORCING_BT = 4*F, OBC_VERT_ADVEL_T = 4*F, OBC_VERT_ADVEL_U = 4*F, OBC_ENHANCE_VISC_BACK = NONE NONE NONE NONE , OBC_ENHANCE_DIFF_BACK = NONE NONE NONE NONE , ENH_PNTS = 4*1, ENH_FAC_V = 4*0.900000000000000 , ENH_FAC_D = 4*1.00000000000000 , OBC_RELAX_TRACER = 40*F, OBC_FLOW_RELAX = 40*1, OBC_CONSIDER_SOURCES = 40*F, OBC_TRACER_NO_INFLOW = 40*F, REL_COEF_TRACER_IN = 40*0.000000000000000E+000 , REL_COEF_TRACER_OUT = 40*0.000000000000000E+000 , FILENAME_TRACER = INPUT/obc_tr.nc INPUT/obc_tr.nc INPUT/obc_tr.nc INPUT/obc_tr.nc INPUT/obc_tr.nc INPUT/obc_tr.nc INPUT/obc_tr.nc INPUT/obc_tr.nc none none none none none none none none none none none none none none none none none none none none none none none none none none none none none none none none , FIELDNAME_TRACER = temp_obc temp_obc temp_obc temp_obc salt_obc salt_obc salt_obc salt_obc none none none none none none none none none none none none none none none none none none none none none none none none none none none none none none none none , DEBUG_PHASE_SPEED = F, DEBUG_THIS_MODULE = F, OBC_DAMP_NEWTON = 4*F, DAMP_FACTOR = 4*1.00000000000000 / Number of wet ocean tracer points = 2665319 Number of wet ocean velocity points = 2524992 Number of computed ocean tracer points = 5400000 Wet ocean volume with eta_t=0.0 (T-cells) = 1.29155143404867584E+18 m^3 (not bit reproducible) Ocean surface area (T-cells) = 3.61335993807307500E+14 m^2 (not bit reproducible) Wet ocean volume with eta_u=0.0 (U-cells) = 1.18684686612431642E+18 m^3 (not bit reproducible) Wet ocean surface area (U-cells) = 3.48819199235927937E+14 m^2 (not bit reproducible) Wet ocean + masked-out (land) surface area (T-cells) = 5.04487703379211250E+14 m^2 (not bit reproducible) Wet ocean + masked-out (land) surface area (U-cells) = 5.04719695457285187E+14 m^2 (not bit reproducible) &OCEAN_TRACER_UTIL_NML REBIN_ONTO_RHO_ALL_VALUES = T, DEBUG_DIAGNOSE_MASS_OF_LAYER = F, EPSLN_DIAGNOSE_MASS_OF_LAYER = 1.000000000000000E-005 / Note: ocean_tracer_util: rebin_onto_rho will include density values outside bounds range. &OCEAN_CORIOLIS_NML DEBUG_THIS_MODULE = F, USE_THIS_MODULE = T, ACOR = 0.500000000000000 / ==>Note: Coriolis on Bgrid computed semi-implicitly to remove inertial time step constraint. ==> Note: 2*pi timesteps/(min inertial period) implies a maximum dtuv for time-explicit Coriolis = 6856. sec. &OCEAN_VELOCITY_NML DEBUG_THIS_MODULE = F, WRITE_A_RESTART = T, MAX_CGINT = 1.00000000000000 , ZERO_TENDENCY = F, ZERO_TENDENCY_EXPLICIT_A = F, ZERO_TENDENCY_EXPLICIT_B = F, ZERO_TENDENCY_IMPLICIT = F, TRUNCATE_VELOCITY = T, TRUNCATE_VERBOSE = T, TRUNCATE_VELOCITY_LAT = 0.000000000000000E+000, TRUNCATE_VELOCITY_VALUE = 2.00000000000000 , ADAMS_BASHFORTH_THIRD = T, ADAMS_BASHFORTH_EPSILON = 0.600000000000000 , USE_CONSTANT_VELOCITY = F, CONSTANT_U = 0.000000000000000E+000, CONSTANT_V = 0.000000000000000E+000, UPDATE_VELOCITY_VIA_UPRIME = T / ==>Warning: truncate_velocity=.true. Model will truncate baroclinc velocity so that max horz velocity magnitude is (m/s) 2.000 Truncation occurs for regions poleward of the latitude 0.000 This option may be useful during the spin-up phase of an experiment. It is also of use for polar filtering. ==>Note from ocean_velocity_mod: use of twolevel time_tendency necessitates an Adams-Bashforth treatment of velocity advection. Using 3rd order Adams-Bashforth for velocity advection. This is the MOM default. NOTE from PE 0: ==>update_velocity_via_uprime=.true., so keep udrho from external mode solver. Baroclinic time step stability most nearly violated at U-cell (i,j) = ( 198, 246), (lon,lat) = ( -82.00, 65.14). The number of kmu-levels at this point is 22 The dxu grid distance (m) at this point is 0.467431E+05 The dyu grid distance (m) at this point is 0.159462E+05 Due to a specified maximum baroclinic gravity wave speed of 1.00 m/s. "dtuv" must be less than 15092. sec. "dtuv" = 3600. sec. NOTE from PE 0: ==> From ocean_velocity_mod: Initializing velocity to zero since Time%init=.true. and did not find INPUT/ocean_velocity.res.nc. ===Initial velocity checksums ==> yyyy/mm/dd hh:mm:ss = 1/ 1/ 1 0: 0: 0 From ocean_velocity_mod: initial velocity chksum (taup1) [chksum] Zonal velocity 1588930713756969728 [chksum] Meridional velocity 1588930713756969728 [chksum] Advection of u 0 [chksum] Advection of v 0 &OCEAN_BAROTROPIC_NML WRITE_A_RESTART = T, ZERO_TENDENCY = F, ZERO_ETA_IC = F, ZERO_ETA_T = F, ZERO_ETA_U = F, ZERO_CORIOLIS_BT = F, ZERO_NONLINEAR_FORCING_BT = F, ZERO_FORCING_BT = F, ZERO_ETA_TENDENCY = F, BAROTROPIC_TIME_STEPPING_A = T, BAROTROPIC_TIME_STEPPING_B = F, TIDAL_FORCING_M2 = F, TIDAL_FORCING_8 = F, TIDAL_FORCING_IDEAL = F, GEOID_FORCING = F, ALPHAT = 0.948000000000000 , PRED_CORR_GAMMA = 0.200000000000000 , SMOOTH_ETA_T_BT_LAPLACIAN = F, SMOOTH_ETA_T_BT_BIHARMONIC = F, SMOOTH_ETA_T_LAPLACIAN = T, SMOOTH_ETA_T_BIHARMONIC = F, SMOOTH_ANOMPB_BT_LAPLACIAN = F, SMOOTH_ANOMPB_BT_BIHARMONIC = F, SMOOTH_PBOT_T_LAPLACIAN = T, SMOOTH_PBOT_T_BIHARMONIC = F, SMOOTH_PBOT_T_BIHARMONIC_LEGACY = F, SMOOTH_ETA_DIAG_LAPLACIAN = T, SMOOTH_ETA_DIAG_BIHARMONIC = F, VEL_MICOM_LAP = 5.000000000000000E-002, VEL_MICOM_LAP_DIAG = 0.200000000000000 , VEL_MICOM_BIH = 1.000000000000000E-002, VEL_MICOM_BIH_DIAG = 0.100000000000000 , TRUNCATE_ETA = F, VERBOSE_TRUNCATE = T, ETA_MAX = 8.00000000000000 , FRAC_CRIT_CELL_HEIGHT = 0.200000000000000 , VERBOSE_INIT = T, DEBUG_THIS_MODULE = F, DIAG_STEP = 4320, ETA_OFFSET = 1.000000000000000E-012, PBOT_OFFSET = 1.000000000000000E-012, INITSUM_WITH_BAR_MOM4P0 = F, INITSUM_WITH_BAR_MOM4P1 = T, IDEAL_INITIAL_ETA = F, IDEAL_INITIAL_ETA_AMPLITUDE = 5.00000000000000 , IDEAL_INITIAL_ETA_XWIDTH = 100000.000000000 , IDEAL_INITIAL_ETA_YWIDTH = 100000.000000000 , UDRHO_BT_LAP = F, UDRHO_BT_BIH = F, UDRHO_LAP = F, UDRHO_BIH = F, UDRHO_LAP_VEL_MICOM = 5.000000000000000E-002, UDRHO_BIH_VEL_MICOM = 1.000000000000000E-002, BAROTROPIC_HALO = 10, DO_BITWISE_EXACT_SUM = F, USE_LEGACY_BAROTROPIC_HALOS = F / horz diff flux domain decomposition whalo = 1, ehalo = 1, shalo = 1, nhalo = 1 X-AXIS = 23 23 23 23 22 22 22 22 22 22 22 22 23 23 23 23 Y-AXIS = 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 NOTE from PE 0: mpp_domains_define.inc(mpp_define_io_domain): io domain will not be defined for horz diff flux when one or both entry of io_layout is not positive barotropic domain domain decomposition whalo = 10, ehalo = 10, shalo = 10, nhalo = 10 X-AXIS = 23 23 23 23 22 22 22 22 22 22 22 22 23 23 23 23 Y-AXIS = 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 NOTE from PE 0: mpp_domains_define.inc(mpp_define_io_domain): io domain will not be defined for barotropic domain when one or both entry of io_layout is not positive NOTE from PE 0: Using barotropic predictor-corrector for integrating barotropic dynamics. Predictor-Corrector time filter on barotropic dynamics has value= 0.20 Updating eta_t or pbot_t using a big time step as in MOM4.0. Not recommended for OBC applications. Initialise sum of barotropic sea level with eta_t or pbot_t. This is the default. ==> Note: The barotropic dynamics integrate 160 timesteps for every one baroclinic timestep. ==>Using smooth_eta_t_laplacian to smooth eta_t. NOTE from PE 0: ==>Note from tidal_forcing_init: tidal_forcing=false, so not adding tidal forcing to external mode. Barotropic stability most nearly violated at T-cell (i,j) = ( 78, 300), (lon,lat) = ( -275.42, 87.21). The number of kmt-levels at this point is 46 The dxt grid spacing (m) at this point is 0.249344E+05 The dyt grid spacing (m) at this point is 0.494923E+05 where the barotropic gravity wave speed is ~242.0 m/s. "dtbt" must be less than 103.000 sec. dtbt = 45.000 sec. &OCEAN_THICKNESS_NML DEBUG_THIS_MODULE = F, DEBUG_THIS_MODULE_DETAIL = F, WRITE_A_RESTART = T, FULL_STEP_TOPOGRAPHY = F, INITIALIZE_ZERO_ETA = F, ENFORCE_POSITIVE_DZT = F, DEPTH_MIN_FOR_SIGMA = 1.000000000000000E-002, THICKNESS_METHOD = energetic , READ_RHO0_PROFILE = F, THICKNESS_DZT_MIN = 1.00000000000000 , THICKNESS_DZT_MIN_INIT = 2.00000000000000 , RESCALE_MASS_TO_GET_HT_MOD = F, PBOT0_SIMPLE = F, EPSILON_INIT_THICKNESS = 1.000000000000000E-005, READ_RESCALE_RHO0_MASK = F, RESCALE_RHO0_MASK_GFDL = F, RESCALE_RHO0_BASIN_LABEL = 7.00000000000000 , RESCALE_RHO0_VALUE = 0.750000000000000 , LINEAR_FREE_SURFACE = F, MAX_NUM_BAD_PRINT = 25, UPDATE_DZWU_K0 = T / ==>Note: running ocean_thickness with thickness_method=energetic. &OCEAN_OPERATORS_NML USE_LEGACY_DIV_UD = F / horz diff flux domain decomposition whalo = 1, ehalo = 1, shalo = 1, nhalo = 1 X-AXIS = 23 23 23 23 22 22 22 22 22 22 22 22 23 23 23 23 Y-AXIS = 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 NOTE from PE 0: mpp_domains_define.inc(mpp_define_io_domain): io domain will not be defined for horz diff flux when one or both entry of io_layout is not positive &OCEAN_TRACER_NML DEBUG_THIS_MODULE = F, ZERO_TENDENCY = F, ZERO_TRACER_SOURCE = F, WRITE_A_RESTART = T, OCEAN_TPM_DEBUG = F, TMASK_LIMIT_TS_SAME = T, REMAP_DEPTH_TO_S_INIT = F, INFLOW_NBOUNDARY = F, INTERPOLATE_TPROG_TO_PBOTT = T, INTERPOLATE_TDIAG_TO_PBOTT = F, LIMIT_AGE_TRACER = T, AGE_TRACER_MAX_INIT = 0.000000000000000E+000, FRAZIL_HEATING_BEFORE_VPHYSICS = F, FRAZIL_HEATING_AFTER_VPHYSICS = T, COMPUTE_TMASK_LIMIT_ON = T, USE_TEMPSALT_CHECK_RANGE = T / ==>Note: frazil heating called after vertical physics and after boundary fluxes. This is the recommended method. NOTE from PE 0: ==>Note from ocean_tracer_mod(ocean_prog_tracer_init): Synchronous timesteps have been specified (dtts = dtuv). ==>Note from ocean_tpm_util_mod(otpm_set_tracer_package)[ocean_tracer_mod(ocean _prog_tracer_init)]: Processing tracer package required &OCEAN_TEMPSALT_NML DEBUG_THIS_MODULE = F, TEMPERATURE_VARIABLE = conservative_temp , POTTEMP_2ND_ITERATION = T, POTTEMP_EQUAL_CONTEMP = F, T_MIN = -5.00000000000000 , T_MAX = 55.0000000000000 , S_MIN = -1.00000000000000 , S_MAX = 55.0000000000000 , T_MIN_LIMIT = -2.00000000000000 , T_MAX_LIMIT = 32.0000000000000 , S_MIN_LIMIT = 0.000000000000000E+000, S_MAX_LIMIT = 42.0000000000000 , REINIT_TS_WITH_IDEAL = F, REINIT_TS_WITH_IDEAL_EFOLD = 1000.00000000000 , REINIT_TS_WITH_IDEAL_TVALUE = 10.0000000000000 , REINIT_TS_WITH_IDEAL_SVALUE = 30.0000000000000 , TEOS10 = F / ==>Note from ocean_tempsalt_mod: MOM prognostic temp = conservative temperature. MOM diagnostic temp = potential temperature. ==>Note from ocean_tpm_util_mod(otpm_set_prog_tracer)[ocean_tempsalt_mod/ocean_ tempsalt_init]: Processing prog tracer temp ==>Note from ocean_tpm_util_mod(otpm_set_prog_tracer)[ocean_tempsalt_mod/ocean_ tempsalt_init]: Processing prog tracer salt ==>Note from ocean_tpm_util_mod(otpm_set_diag_tracer)[ocean_tempsalt_mod/ocean_ tempsalt_init]: Processing diag tracer pot_temp &OCEAN_FRAZIL_NML USE_THIS_MODULE = T, DEBUG_THIS_MODULE = F, FREEZING_TEMP_SIMPLE = T, FREEZING_TEMP_PRETEOS10 = F, FREEZING_TEMP_TEOS10 = F, FRAZIL_FACTOR = 1.00000000000000 , AIR_SATURATED_WATER = T, FRAZIL_ONLY_IN_SURFACE = T / NOTE from PE 0: ==>Note from ocean_frazil_mod: USING frazil heating. ==>Note: Using simple equation for seawater freezing temperature. Assuming that frazil forms only in the surface(k=1) ocean grid cell. Setting gauge pressure to zero when computing seawater freezing temperature. ==>Note from ocean_tpm_util_mod(otpm_set_diag_tracer)[ocean_frazil_mod/ocean_fr azil_init]: Processing diag tracer frazil ==>Note from ocean_frazil_mod: using frazil_factor= 1.00 ==>Note from ocean_tpm_util_mod(otpm_set_tracer_package)[ocean_passive_mod(ocea n_passive_init)]: Processing tracer package ocean_passive ==>Note from ocean_passive_mod(ocean_passive_init): No instances of passive tracers in field_table. ==>Note: NOT running with idealized passive tracers. NOTE from PE 0: ==>Note: ocean_passive_mod: NOT using idealized passive tracer module. ==>Note from ocean_tpm_util_mod(otpm_set_tracer_package)[ocean_residency_mod(oc ean_residency_init)]: Processing tracer package ocean_residency ==>Note from ocean_residency_mod(ocean_residency_init): No instances ==>Note from ocean_tpm_util_mod(otpm_set_tracer_package)[ocean_age_tracer_mod(o cean_age_tracer_init)]: Processing tracer package ocean_age_tracer ==>Note from ocean_age_tracer_mod(ocean_age_tracer_init): 1 instances ==>Note from ocean_tpm_util_mod(otpm_set_prog_tracer)[ocean_age_tracer_mod(ocea n_age_tracer_init)]: Processing prog tracer age_global ==>Note from fm_util_mod(fm_util_start_namelist)[ocean_age_tracer_mod(ocean_age _tracer_init)]: Processing namelist ocean_age_tracer/global ==>Note from ocean_tpm_util_mod(otpm_set_tracer_package)[transport_matrix_mod(t ransport_matrix_init)]: Processing tracer package transport_matrix ==>Note from transport_matrix_mod(transport_matrix_init): No instances Dumping tracer_packages tracer tree tracer_packages/ ocean_age_tracer/ names = 'global' const_init_tracer = T horizontal-advection-scheme = 'mdppm' vertical-advection-scheme = 'mdppm' ppm_hlimiter = 3 ppm_vlimiter = 3 restart_file = 'ocean_age.res.nc' min_tracer_limit = 0.000000000000000E+000 units = 'yr' min_range = 0.000000000000000E+000 max_range = 1.000000000000000E+020 flux_units = 'm' max_tracer_limit = 1.000000000000000E+020 required/ names = NULL ocean_passive/ names = NULL units = 'dimensionless' conversion = 1.00000000000000 offset = 0.000000000000000E+000 min_tracer = -1000000.00000000 max_tracer = 1000000.00000000 min_range = -10.0000000000000 max_range = 100.000000000000 restart_file = 'ocean_passive.res.nc' psom_limit = T flux_units = 'dimensionless' min_flux_range = -1.000000000000000E+016 max_flux_range = 1.000000000000000E+016 min_tracer_limit = -0.100000000000000 max_tracer_limit = 1.00000000000000 vertical-advection-scheme = 'mdppm' horizontal-advection-scheme = 'mdppm' ocean_residency/ names = NULL units = 'yr' restart_file = 'ocean_residency.res.nc' flux_units = 'm' min_tracer_limit = 0.000000000000000E+000 max_tracer_limit = 1.000000000000000E+020 transport_matrix/ names = NULL restart_file = 'transport_matrix.res.nc' Dumping prog_tracers tracer tree prog_tracers/ temp/ horizontal-advection-scheme = 'mdppm' vertical-advection-scheme = 'mdppm' restart_file = 'ocean_temp_salt.res.nc' ppm_hlimiter = 3 ppm_vlimiter = 3 longname = 'Conservative temperature' units = 'deg_C' type = '' conversion = 3992.10322329649 offset = 273.150000000000 min_tracer = -5.00000000000000 max_tracer = 55.0000000000000 min_range = -10.0000000000000 max_range = 500.000000000000 use_only_advection = F const_init_tracer = F const_init_value = 0.000000000000000E+000 psom_limit = F mdt_scheme = 1 flux_units = 'Watts/m^2' min_flux_range = -1.000000000000000E+016 max_flux_range = 1.000000000000000E+016 min_tracer_limit = -2.00000000000000 max_tracer_limit = 32.0000000000000 salt/ horizontal-advection-scheme = 'mdppm' vertical-advection-scheme = 'mdppm' restart_file = 'ocean_temp_salt.res.nc' ppm_hlimiter = 3 ppm_vlimiter = 3 longname = 'Practical Salinity' units = 'psu' type = '' conversion = 1.000000000000000E-003 offset = 0.000000000000000E+000 min_tracer = -1.00000000000000 max_tracer = 55.0000000000000 min_range = -10.0000000000000 max_range = 100.000000000000 use_only_advection = F const_init_tracer = F const_init_value = 0.000000000000000E+000 psom_limit = F mdt_scheme = 1 flux_units = 'kg/(sec*m^2)' min_flux_range = -100000.000000000 max_flux_range = 100000.000000000 min_tracer_limit = 0.000000000000000E+000 max_tracer_limit = 42.0000000000000 age_global/ longname = 'Age (global)' units = 'yr' type = '' conversion = 1.00000000000000 offset = 0.000000000000000E+000 min_tracer = -1.000000000000000E+020 max_tracer = 1.000000000000000E+020 min_range = 0.000000000000000E+000 max_range = 1.000000000000000E+020 use_only_advection = F restart_file = 'ocean_age.res.nc' const_init_tracer = T const_init_value = 0.000000000000000E+000 psom_limit = F ppm_hlimiter = 3 ppm_vlimiter = 3 mdt_scheme = 1 flux_units = 'm' min_flux_range = 1.00000000000000 max_flux_range = 0.000000000000000E+000 min_tracer_limit = 0.000000000000000E+000 max_tracer_limit = 1.000000000000000E+020 vertical-advection-scheme = 'mdppm' horizontal-advection-scheme = 'mdppm' Dumping namelists tracer tree namelists/ ocean_age_tracer/ global/ slat = -90.0000000000000 nlat = 90.0000000000000 wlon = 0.000000000000000E+000 elon = 360.000000000000 coastal_only = F t_mask[1] = T t_mask[2] = T t_mask[3] = T t_mask[4] = T t_mask[5] = T t_mask[6] = T t_mask[7] = T t_mask[8] = T t_mask[9] = T t_mask[10] = T t_mask[11] = T t_mask[12] = T age_tracer_type = 'not used' ==> Note from ocean_tracer_mod: prognostic temperature = conservative temperature. diagnostic temperature = potential temperature. ==>Note from ocean_tracer_mod(ocean_prog_tracer_init): Reading prognostic tracer initial conditions or restarts Initializing tracer number 1 at time level tau. This tracer is called temp Reading restart for prog tracer temp from file ocean_temp_salt.res.nc After reading ic, linearly interpolate temp to partial cell bottom. Completed initialization of tracer temp at time level tau Initializing tracer number 2 at time level tau. This tracer is called salt Reading restart for prog tracer salt from file ocean_temp_salt.res.nc After reading ic, linearly interpolate salt to partial cell bottom. Completed initialization of tracer salt at time level tau Initializing tracer number 3 at time level tau. This tracer is called age_global Initializing the tracer age_global to the constant 0.000000000000000E+000 Completed initialization of tracer age_global at time level tau ==>Note from ocean_tracer_mod(ocean_prog_tracer_init): finished reading prognostic tracer restarts. ==>Note from ocean_tpm_util_mod(otpm_set_diag_tracer)[ocean_shortwave_mod(ocean _irradiance_init)]: Processing diag tracer irr ==>Note from ocean_tracer_mod(ocean_diag_tracer_init): 3 diagnostic tracers requested. Dumping ocean diag field tree after reading diag tracer tree diag_tracers/ pot_temp/ longname = 'Potential temperature' units = 'deg_C' type = '' conversion = 3992.10322329649 offset = 273.150000000000 min_tracer = -5.00000000000000 max_tracer = 55.0000000000000 min_range = -10.0000000000000 max_range = 500.000000000000 restart_file = 'ocean_pot_temp.res.nc' const_init_tracer = T const_init_value = 0.000000000000000E+000 frazil/ longname = 'frazil heating' units = 'J/m^2' type = '' conversion = 1.00000000000000 offset = 0.000000000000000E+000 min_tracer = 0.000000000000000E+000 max_tracer = 1.000000000000000E+020 min_range = -10.0000000000000 max_range = 100.000000000000 restart_file = 'ocean_frazil.res.nc' const_init_tracer = T const_init_value = 0.000000000000000E+000 irr/ longname = 'Irradiance' units = 'Watts/m^2' type = '' conversion = 1.00000000000000 offset = 0.000000000000000E+000 min_tracer = -1.000000000000000E+020 max_tracer = 1.000000000000000E+020 min_range = 1.00000000000000 max_range = 0.000000000000000E+000 restart_file = '' const_init_tracer = T const_init_value = 0.000000000000000E+000 ==>Note from ocean_tracer_mod(ocean_diag_tracer_init): Reading diagnostic tracer initial conditions and/or restarts Initializing tracer number 1 at time level tau. This tracer is called pot_temp Initializing diagnostic tracer pot_temp to constant 0.000000000000000E+000 Initializing tracer number 2 at time level tau. This tracer is called frazil Initializing diagnostic tracer frazil to constant 0.000000000000000E+000 Initializing tracer number 3 at time level tau. This tracer is called irr Skipping tracer irr ==>Note from ocean_tracer_mod(ocean_diag_tracer_init): Finished reading diagnostic tracer restarts. &OCEAN_ADVECTION_VELOCITY_NML DEBUG_THIS_MODULE = F, MAX_ADVECTION_VELOCITY = 0.500000000000000 , INFLOW_NBOUNDARY = F, READ_ADVECTION_VELOCITY = F, READ_ADVECTION_TRANSPORT = F, CONSTANT_ADVECTION_VELOCITY = F / Note: Advection stability most nearly violated at T-cell (i,j) = ( 198, 246), (lon,lat) = ( -82.501, 65.069). Assuming a maximum advection velocity of 0.50 m/s, Linear stability requires max(dtuv,dtts) be less than 7709.20 sec. Model is now using (dtuv,dtts) = ( 3600.00, 3600.00) sec. &OCEAN_DENSITY_NML S_TEST = 20.0000000000000 , T_TEST = 20.0000000000000 , P_TEST = 1000.00000000000 , PRESS_STANDARD = 0.000000000000000E+000, SN_TEST = 35.0000000000000 , TN_TEST = 20.0000000000000 , EOS_LINEAR = F, ALPHA_LINEAR_EOS = 0.255000000000000 , BETA_LINEAR_EOS = 0.000000000000000E+000, EOS_PRETEOS10 = T, EOS_TEOS10 = F, POTRHO_PRESS = 2000.00000000000 , POTRHO_MIN = 1028.00000000000 , POTRHO_MAX = 1038.00000000000 , NEUTRALRHO_MIN = 1020.00000000000 , NEUTRALRHO_MAX = 1030.00000000000 , LAYER_NK = 80, THETA_MIN = -2.00000000000000 , THETA_MAX = 30.0000000000000 , DEBUG_THIS_MODULE = F, WRITE_A_RESTART = T, RHO0_DENSITY = F, DENSITY_EQUAL_POTRHO = F, BUOYFREQ_SMOOTH_VERT = T, NUM_121_PASSES = 1, EPSLN_DRHODZ = 1.000000000000000E-010, MASK_DOMAIN_RESTART = F, DO_BITWISE_EXACT_SUM = F, DRHODZ_DIAG_STABLE = T, EPSLN_DRHODZ_DIAG = 1.000000000000000E-010, GRAD_NRHO_LRPOTRHO_COMPUTE = F, GRAD_NRHO_LRPOTRHO_MAX = 10.0000000000000 , GRAD_NRHO_LRPOTRHO_MIN = 1.00000000000000 , NEUTRAL_DENSITY_OMEGA = F, NEUTRAL_DENSITY_POTRHO = T, SMOOTH_STRATIFICATION_FACTOR = F, UPDATE_DIAGNOSTIC_FACTORS = F, SMAX_DIAG = -1.00000000000000 , SMAX_MIN_IN_COLUMN = F / ==> Note: USING preTEOS10 EOS, as relevant for realistic ocean climate simulations. Subtracting standard atmosphere of 0.000000 dbar for EOS calculation. ==> Note: Computing EOS assuming prognostic temp = conservative temperature. ==> Note: Computing EOS assuming prognostic salinity = practical salinity. ==>Note: The Boussinesq rho0 density has a value of (kg/m^3) 1035.00000000000 ==> Note: Computing diagnostic neutral_rho as potential density referenced to pressure potrho_press. ==> Note: Enforcing drhodz_diag < 0, so to use stable stratification for certain diagnostic purposes. ==> Note: Diagnostic factors are NOT computed. So if enable watermass diagnostics, they will be corrupted. preTEOS10 EQUATION OF STATE TEST VALUES s_test(psu) = 20.00, t_test(C) = 20.00, p_test(dbar) = 1000.00 rho ( 20.00, 20.00, 1000.00) = 0.1017842890411976E+04 kg/m^3 diff from JMFWG = 0.5684341886080801E-12 kg/m^3 alpha( 20.00, 20.00, 1000.00) = 0.2436057013634663E-03 1/C diff from JMFWG = 0.1409462824231156E-17 1/C beta ( 20.00, 20.00, 1000.00) = 0.7314818108935242E-03 1/psu squared sound speed ( 20.00, 20.00, 1000.00) = 0.2311451354560629E+03 (m/s)^2 diff from JMFWG = -.6505213034913027E-18 1/psu NEUTRAL DENSITY EQUATION TEST VALUES sn_test(psu) = 35.00, tn_test(C) = 20.00 rho ( 35.00, 20.00) = 0.1024438639277630E+04 kg/m^3 diff from Klocker and McDougall test = 0.0000000000000000E+00 kg/m^3 Initialising salinity for use in density calculation ==>Note: From ocean_density_mod: Boussinesq reference density rho0(kg/m3) = 0.103500000000E+04 Initial rho_average(kg/m3) = 0.103735353585E+04 Since rho0 .ne. rho_average, consider changing rho0 in ocean_parameters.F90 to be equal to rho_average for better accuracy. From ocean_density_mod: density chksums from ocean_density_init yyyy/mm/dd hh:mm:ss = 1/ 1/ 1 0: 0: 0 [chksum] rho(taup1) 5244488794857896540 [chksum] pressure_at_depth 5463872455083449137 [chksum] denominator_r -3619163387261538046 [chksum] drhodT 0 [chksum] drhodS 0 [chksum] drhodz_zt -5863330072026482088 &OCEAN_BLOB_NML BLOB_SMALL_MASS = 1000.00000000000 , DEBUG_THIS_MODULE = F, REALLY_DEBUG = F, DO_BITWISE_EXACT_SUM = F, BITWISE_REPRODUCTION = F, MAX_PROP_THICKNESS = 0.700000000000000 / ==>Note: NOT using the Lagrangian buoyancy blobs scheme. &OCEAN_PRESSURE_NML DEBUG_THIS_MODULE = F, ZERO_PRESSURE_FORCE = F, ZERO_CORRECTION_TERM_GRAD = F, ZERO_DIAGONAL_PRESS_GRAD = F, ZERO_ETA_OVER_H_ZSTAR_PRESSURE = F / ==>NOTE: Running MOM with finite difference formulation of pressure force. &OCEAN_VERT_MIX_NML DEBUG_THIS_MODULE = F, VERT_MIX_SCHEME = kpp_mom4p1, VERBOSE_INIT = T, AIDIF = 1.00000000000000 , VERT_DIFF_BACK_VIA_MAX = T, USE_EXPLICIT_VERT_DIFFUSE = T, USE_DIFF_CBT_TABLE = F, LINEAR_TAPER_DIFF_CBT_TABLE = F, BRYAN_LEWIS_DIFFUSIVITY = F, BRYAN_LEWIS_LAT_DEPEND = T, BRYAN_LEWIS_LAT_TRANSITION = 35.0000000000000 , AFKPH_90 = 0.750000000000000 , DFKPH_90 = 0.950000000000000 , SFKPH_90 = 4.500000000000000E-005, ZFKPH_90 = 250000.000000000 , AFKPH_00 = 0.650000000000000 , DFKPH_00 = 1.15000000000000 , SFKPH_00 = 4.500000000000000E-005, ZFKPH_00 = 250000.000000000 , VERT_VISC_BACK = F, VISC_CBU_BACK_MAX = 1.000000000000000E-002, VISC_CBU_BACK_MIN = 1.000000000000000E-003, VISC_CBU_BACK_ZMID = 50.0000000000000 , VISC_CBU_BACK_ZWID = 30.0000000000000 , HWF_DIFFUSIVITY = F, HWF_DEPTH_TRANSITION = 25000000.0000000 , HWF_MIN_DIFFUSIVITY = 2.000000000000000E-006, HWF_30_DIFFUSIVITY = 2.000000000000000E-005, HWF_N0_2OMEGA = 20.0000000000000 , HWF_DIFFUSIVITY_3D = F, DIFF_CBT_TANH = F, DIFF_CBT_TANH_MAX = 1.000000000000000E-003, DIFF_CBT_TANH_MIN = 2.000000000000000E-005, DIFF_CBT_TANH_ZMID = 150.000000000000 , DIFF_CBT_TANH_ZWID = 30.0000000000000 , QUEBEC_2009_10_BUG = F, VMIX_RESCALE_NONBOUSS = F, VMIX_SET_MIN_DISSIPATION = F, VMIX_MIN_DISS_CONST = 1.000000000000000E-007, VMIX_MIN_DISS_BVFREQ_SCALE = 5.999999999999999E-004, VMIX_MIN_DISS_FLUX_RI_MAX = 0.200000000000000 , SMOOTH_RHO_N2 = T, NUM_121_PASSES = 1 / &OCEAN_VERT_UTIL_NML DEBUG_THIS_MODULE = F, SMOOTH_N2 = T, SMOOTH_RI_NUMBER = T, NUM_N2_SMOOTH = 1, NUM_RI_SMOOTH = 1 / NOTE from PE 0: ==>Warning: ocean_vert_mix_init NO table for enhanced diff_cbt. No diffusivities read. &OCEAN_VERT_TIDAL_NML USE_THIS_MODULE = T, USE_LEGACY_METHODS = F, DEBUG_THIS_MODULE = F, USE_WAVE_DISSIPATION = T, USE_DRAG_DISSIPATION = T, READ_ROUGHNESS = T, READ_TIDE_SPEED = T, DEFAULT_ROUGHNESS_LENGTH = 25.0000000000000 , DEFAULT_TIDE_SPEED = 1.000000000000000E-002, SHELF_DEPTH_CUTOFF = 160.000000000000 , DECAY_SCALE = 300.000000000000 , ROUGHNESS_SCALE = 20000.0000000000 , TIDAL_DISS_EFFICIENCY = 0.333330000000000 , MIXING_EFFICIENCY = 0.200000000000000 , MIXING_EFFICIENCY_N2DEPEND = T, MUNK_ANDERSON_P = 0.250000000000000 , MUNK_ANDERSON_SIGMA = 3.00000000000000 , DRAG_DISSIPATION_EFOLD = T, DRAG_DISSIPATION_TIDE_PERIOD = 43200.0000000000 , DRAG_MASK_DEEP = T, DRAG_MASK_DEEP_RATIO = 0.100000000000000 , BOTTOM_DRAG_CD = 2.400000000000000E-003, DRHODZ_MIN = 1.000000000000000E-012, SPEED_MIN = 5.000000000000000E-003, BACKGROUND_DIFFUSIVITY = 5.000000000000000E-006, BACKGROUND_VISCOSITY = 1.000000000000000E-004, MAX_WAVE_DIFFUSIVITY = 1.000000000000000E-002, MAX_DRAG_DIFFUSIVITY = 1.000000000000000E-002, SMOOTH_BVFREQ_BOTTOM = T, VEL_MICOM_SMOOTH = 0.200000000000000 , SMOOTH_RHO_N2 = T, NUM_121_PASSES = 1, WAVE_DIFFUSIVITY_MONOTONIC = T, TIDE_SPEED_DATA_ON_T_GRID = T, READING_ROUGHNESS_AMP = T, READING_ROUGHNESS_LENGTH = F, READ_WAVE_DISSIPATION = F, FIXED_WAVE_DISSIPATION = F, WAVE_ENERGY_FLUX_MAX = 0.100000000000000 , USE_LEEWAVE_DISSIPATION = F, READ_LEEWAVE_DISSIPATION = F, DRAG_DISSIPATION_USE_CDBOT = F / NOTE from PE 0: ==>Note: USING ocean_vert_tidal_mod Using Simmons etal scheme to compute dia-surface diffusivity and viscosity based on internal wave breaking. Using Lee etal scheme to compute dia-surface diffusivity and viscosity based on barotropic tide drag on bottom. NOT using Nikurashin scheme for dia-surface diffusivity and viscosity. ==>ocean_vert_tidal_mod: Completed read of topographic roughness amplitude on T -grid. ==>Note: NOT reading wave dissipation for ocean_vert_tidal_mod. ==>Note: NOT reading leewave dissipation for ocean_vert_tidal_mod. ==>ocean_vert_tidal_mod: Completed read of tide_speed on T-grid. ==>Note from ocean_vert_tidal: using constant bottom drag coefficient for tide drag_dissipation scheme. ==>Note from ocean_vert_mix: KPP_mom4p1 for vert diffusivity, viscosity, nonlocal, and barotropic tide drag. &OCEAN_VERT_KPP_MOM4P1_NML USE_THIS_MODULE = T, SHEAR_INSTABILITY = T, DOUBLE_DIFFUSION = T, DIFF_CBT_IW = 0.000000000000000E+000, VISC_CBU_IW = 0.000000000000000E+000, VISC_CBU_LIMIT = 5.000000000000000E-003, DIFF_CBT_LIMIT = 5.000000000000000E-003, VISC_CON_LIMIT = 0.100000000000000 , DIFF_CON_LIMIT = 0.100000000000000 , CONCV = 1.80000000000000 , RICR = 0.300000000000000 , NON_LOCAL_KPP = T, SMOOTH_BLMC = F, LGAM = 1.04000000000000 , CW_0 = 0.150000000000000 , L_SMYTH = 2.00000000000000 , LTMAX = 5.00000000000000 , WSTFAC = 0.600000000000000 , KL_MIN = 2, KBL_STANDARD_METHOD = F, DEBUG_THIS_MODULE = F, LIMIT_WITH_HEKMAN = T, LIMIT_GHATS = F, HBL_WITH_RIT = F, RADIATION_LARGE = F, RADIATION_ZERO = F, RADIATION_IOW = F, USE_SBL_BOTTOM_FLUX = F, WSFC_COMBINE_RUNOFF_CALVE = T, BVF_FROM_BELOW = F, VARIABLE_VTC = F, USE_MAX_SHEAR = F, LINEAR_HBL = T, CALC_VISC_ON_CGRID = F, SMOOTH_RI_KMAX_EQ_KMU = T, DO_LANGMUIR = F / ==> NOTE: USING KPP vertical mixing scheme. ==> NOTE: KPP is typically run with penetrative shortwave heating. ==> NOTE: KPP is typically run with a seasonal and/or diurnal cycle. ==>Note from ocean_vert_kpp_mom4p1_mod: using forward time step for vert-frict of (secs) 3600.00 ==>Note from ocean_vert_kpp_mom4p1_mod: using forward time step for vert-diff of (secs) 3600.00 ==> NOTE from ocean_vert_kpp_mom4p1_mod: adjust kbl to hbl with the non-standard method. ==>WARNING from ocean_vert_kpp_mom4p1_mod: change kl_min to 1 to avoid negative mixing coefficients with low wind stress. ==> NOTE from ocean_vert_kpp_mom4p1_mod: Find BVF from a backward derivatives. ==> NOTE from ocean_vert_kpp_mom4p1_mod: Diagnose hbl with constant concv. ==> NOTE from ocean_vert_kpp_mom4p1_mod: Use average shear around a tracer cell for diagnostics of hbl. ==> NOTE from ocean_vert_kpp_mom4p1_mod: Use linear interpolation to find hbl ==> NOTE from ocean_vert_kpp_mom4p1_mod: Do not limit ghats*diff_cbt to 1. ==> NOTE from ocean_vert_kpp_mom4p1_mod: Limit hbl with hekman for stable case. ==> NOTE from ocean_vert_kpp_mom4p1_mod: Interpolate viscosity to c-grid. ==> NOTE from ocean_vert_kpp_mom4p1_mod: Leave full sw-radiation in non-local surface flux. Computing vertical mixing from shear instability in KPP module. &OCEAN_BIH_TRACER_NML USE_THIS_MODULE = F, ABIH = 0.000000000000000E+000, TRACER_MIX_MICOM = F, VEL_MICOM = 0.000000000000000E+000, READ_DIFFUSIVITY_MASK = F, HORZ_Z_DIFFUSE = F, HORZ_S_DIFFUSE = T / ==>Note from ocean_bih_tracer_mod: NOT using this module. &OCEAN_LAP_TRACER_NML USE_THIS_MODULE = F, ALAP = 0.000000000000000E+000, TRACER_MIX_MICOM = F, VEL_MICOM = 0.000000000000000E+000, VERBOSE_INIT = T, READ_DIFFUSIVITY_MASK = F, HORZ_Z_DIFFUSE = F, HORZ_S_DIFFUSE = T / ==>Note from ocean_lap_tracer_mod: NOT using this module. &OCEAN_SIGMA_TRANSPORT_NML USE_THIS_MODULE = T, DEBUG_THIS_MODULE = F, TMASK_SIGMA_ON = F, SIGMA_DIFFUSION_ON = T, SIGMA_ADVECTION_ON = F, SIGMA_ADVECTION_SGS_ONLY = F, SIGMA_ADVECTION_CHECK = T, THICKNESS_SIGMA_LAYER = 100.000000000000 , THICKNESS_SIGMA_MAX = 100.000000000000 , THICKNESS_SIGMA_MIN = 100.000000000000 , SIGMA_DIFFUSIVITY = 1000.00000000000 , SIGMA_DIFFUSIVITY_RATIO = 1.000000000000000E-006, TRACER_MIX_MICOM = T, VEL_MICOM = 5.000000000000000E-002, VERBOSE_INIT = T, SIGMA_JUST_IN_BOTTOM_CELL = T, CAMPINGOOSE_MU = 1.000000000000000E-004, CAMPINGOOSE_DELTA = 0.333300000000000 , SIGMA_UMAX = 1.000000000000000E-002, WRITE_A_RESTART = T, SMOOTH_SIGMA_THICKNESS = T, SMOOTH_SIGMA_VELOCITY = T, SMOOTH_VELMICOM = 0.200000000000000 / NOTE from PE 0: ==>Note from ocean_sigma_transport_mod: USING ocean_sigma_transport_mod. ==>Note: ocean_sigma_transport_mod: using forward time step of (secs) 3600.00 ==>Note: ocean_sigma_transport_mod: sigma_diffusion_on=.true. ==>Note: ocean_sigma_transport_mod: sigma_advection_on=.false. ==>Note from ocean_sigma_transport_mod: using sigma_just_in_bottom=.true., as in mom4p0. flux dom sigma domain decomposition whalo = 1, ehalo = 1, shalo = 1, nhalo = 1 X-AXIS = 23 23 23 23 22 22 22 22 22 22 22 22 23 23 23 23 Y-AXIS = 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 NOTE from PE 0: mpp_domains_define.inc(mpp_define_io_domain): io domain will not be defined for flux dom sigma when one or both entry of io_layout is not positive ==>Note: ocean_sigma_transport_mod: initial thickness of sigma layer (m) = 100.0000 ==>Note: ocean_sigma_transport_mod: smooth_sigma_thickness=.true. => diffuse sigma_thickness. Laplacian diffusivity in sigma layer at (isc, 1) = 0.0000000E+00 m^2/s Laplacian diffusivity in sigma layer at (isc, 2) = 0.0000000E+00 m^2/s Laplacian diffusivity in sigma layer at (isc, 3) = 0.0000000E+00 m^2/s Laplacian diffusivity in sigma layer at (isc, 4) = 0.0000000E+00 m^2/s Laplacian diffusivity in sigma layer at (isc, 5) = 0.0000000E+00 m^2/s Laplacian diffusivity in sigma layer at (isc, 6) = 0.0000000E+00 m^2/s Laplacian diffusivity in sigma layer at (isc, 7) = 0.0000000E+00 m^2/s Laplacian diffusivity in sigma layer at (isc, 8) = 0.0000000E+00 m^2/s Laplacian diffusivity in sigma layer at (isc, 9) = 0.0000000E+00 m^2/s Laplacian diffusivity in sigma layer at (isc, 10) = 0.0000000E+00 m^2/s Laplacian diffusivity in sigma layer at (isc, 11) = 0.0000000E+00 m^2/s Laplacian diffusivity in sigma layer at (isc, 12) = 0.0000000E+00 m^2/s Laplacian diffusivity in sigma layer at (isc, 13) = 0.0000000E+00 m^2/s Laplacian diffusivity in sigma layer at (isc, 14) = 0.0000000E+00 m^2/s Laplacian diffusivity in sigma layer at (isc, 15) = 0.0000000E+00 m^2/s Laplacian diffusivity in sigma layer at (isc, 16) = 0.0000000E+00 m^2/s Laplacian diffusivity in sigma layer at (isc, 17) = 0.0000000E+00 m^2/s Laplacian diffusivity in sigma layer at (isc, 18) = 0.0000000E+00 m^2/s Laplacian diffusivity in sigma layer at (isc, 19) = 0.0000000E+00 m^2/s Laplacian diffusivity in sigma layer at (isc, 20) = 0.0000000E+00 m^2/s &OCEAN_NPHYSICS_NML USE_THIS_MODULE = T, DEBUG_THIS_MODULE = F, WRITE_A_RESTART = T, USE_NPHYSICSA = F, USE_NPHYSICSB = F, USE_NPHYSICSC = T / [Note] ocean_nphysics.F90: USING ocean_nphysics_mod. &OCEAN_NPHYSICS_UTIL_NML DEBUG_THIS_MODULE = F, NPHYSICS_UTIL_ZERO_INIT = T, SMAX = 1.000000000000000E-002, SWIDTH = 5.000000000000000E-004, EPSLN_DRHODZ = 1.000000000000000E-030, DRHODZ_MOM4P1 = T, DRHODZ_SMOOTH_HORZ = F, DRHODZ_SMOOTH_VERT = F, NUM_121_PASSES = 1, AREDI = 600.000000000000 , AGM = 600.000000000000 , AREDI_EQUAL_AGM = F, TRACER_MIX_MICOM = F, VEL_MICOM = 0.000000000000000E+000, BRYAN_LEWIS_AREDI = F, AHS = 0.000000000000000E+000, AHB = 0.000000000000000E+000, NEUTRAL_HORZ_MIX_BDY = F, VEL_MICOM_BDY = 0.000000000000000E+000, AH_BDY = 0.000000000000000E+000, AGM_LAT_BANDS = F, AGM_LAT_BANDS_BOUNDARY = -999.000000000000 , AGM_LAT_BANDS_RATIO = 1.00000000000000 , ROSSBY_RADIUS_MAX = 100000.000000000 , ROSSBY_RADIUS_MIN = 15000.0000000000 , AGM_READ_RESTART = F, AGM_CLOSURE = T, AGM_CLOSURE_SCALING = 7.000000000000001E-002, AGM_CLOSURE_MAX = 600.000000000000 , AGM_CLOSURE_MIN = 50.0000000000000 , AGM_CLOSURE_GROWTH_SCALE = 0.500000000000000 , AGM_CLOSURE_LENGTH_FIXED = F, AGM_CLOSURE_LENGTH = 50000.0000000000 , AGM_CLOSURE_LENGTH_ROSSBY = F, AGM_CLOSURE_LENGTH_BCZONE = F, BCZONE_MAX_PTS = 10, AGM_CLOSURE_BCZONE_CRIT_RATE = 1.400000000000000E-006, AGM_CLOSURE_EDEN_GREATBATCH = F, AGM_CLOSURE_EDEN_GAMMA = 0.000000000000000E+000, AGM_CLOSURE_EDEN_LENGTH_CONST = F, AGM_CLOSURE_EDEN_LENGTH = 10000.0000000000 , AGM_CLOSURE_EADY_SMOOTH_VERT = T, AGM_CLOSURE_EADY_SMOOTH_HORZ = T, AGM_CLOSURE_EADY_AVE_MIXED = T, AGM_CLOSURE_EADY_CAP = T, AGM_CLOSURE_BAROCLINIC = T, AGM_CLOSURE_BUOY_FREQ = 4.000000000000000E-003, AGM_CLOSURE_UPPER_DEPTH = 100.000000000000 , AGM_CLOSURE_LOWER_DEPTH = 2000.00000000000 , AGM_CLOSURE_LENGTH_CAP = F, AGM_CLOSURE_LENGTH_MAX = 50000.0000000000 , AGM_SMOOTH_SPACE = F, VEL_MICOM_SMOOTH = 0.200000000000000 , AGM_SMOOTH_TIME = F, AGM_DAMPING_TIME = 45.0000000000000 , AGM_CLOSURE_GRID_SCALING = T, AGM_CLOSURE_GRID_SCALING_POWER = 2.00000000000000 , AREDI_DIFFUSIVITY_GRID_SCALING = F, AGM_CLOSURE_N2_SCALE = F, AGM_CLOSURE_N2_SCALE_COEFF = 1000.00000000000 , AGM_CLOSURE_N2_SCALE_NREF_CST = F, SMAX_GRAD_GAMMA_SCALAR = 1.000000000000000E-002, EPSLN_DRHODZ_DIAGNOSTICS = 1.000000000000000E-007, WDIANEUTRAL_SMOOTH = T, SMOOTH_ETA_TEND_GM90 = F / bczone domain decomposition whalo = 10, ehalo = 10, shalo = 10, nhalo = 10 X-AXIS = 23 23 23 23 22 22 22 22 22 22 22 22 23 23 23 23 Y-AXIS = 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 NOTE from PE 0: mpp_domains_define.inc(mpp_define_io_domain): io domain will not be defined for bczone when one or both entry of io_layout is not positive [Note] ocean_nphysics_util.F90: Computing 2d flow-dependent tracer diffusivity with agm_closure_baroclinic. The maximum allowable diffusivity (m^2/s) is given by .60000E+03 The minimum allowable diffusivity (m^2/s) is given by .50000E+02 Depths (m) between which compute eady growth and baroclinicity = .10000E+03 .20000E+04 [Note] ocean_nphysics_util.F90: Length and time scales set by vertically averaged baroclinicity |grad(rho)|, as well as the constant buoyancy freq(sec^-1) = .40000E-02 and the constant length scale (m) = .50000E+05 [Note] ocean_nphysics.F90: USING ocean_nphysicsC. &OCEAN_NPHYSICSC_NML USE_THIS_MODULE = T, DEBUG_THIS_MODULE = F, DO_NEUTRAL_DIFFUSION = T, DO_GM_SKEWSION = T, NEUTRAL_PHYSICS_LIMIT = T, NEUTRAL_EDDY_DEPTH = T, DM_TAPER = T, GKW_TAPER = F, TMASK_NEUTRAL_ON = T, DIFFUSION_ALL_EXPLICIT = F, TURB_BLAYER_MIN = 50.0000000000000 , GM_SKEWSION_MODES = F, NUMBER_BC_MODES = 2, GM_SKEWSION_BVPROBLEM = T, BVP_BC_MODE = 2, BVP_MIN_SPEED = 0.100000000000000 , BVP_SPEED = 0.000000000000000E+000, BVP_CONSTANT_SPEED = F, BV_FREQ_SMOOTH_VERT = T, NUM_121_PASSES = 1, MIN_BC_SPEED = 1.000000000000000E-006, SMOOTH_PSI = T, EPSLN_BV_FREQ = 1.000000000000000E-012, REGULARIZE_PSI = F, SMAX_PSI = 1.000000000000000E-002, SMOOTH_BC_MODES = F, USE_NEUTRAL_SLOPES_POTRHO = F, NEUTRAL_SLOPES_POTRHO_PRESS = 2000.00000000000 , SMOOTH_ADVECT_TRANSPORT = T, SMOOTH_ADVECT_TRANSPORT_NUM = 2 / [Note] ocean_nphysicsC.F90: USING ocean_nphysicsC. ==> Note from ocean_nphysicsC_mod: using forward time step of (secs) 3600.00 [Note] ocean_nphysicsC.F90: computing neutral diffusion acting on each tracer. [Note] ocean_nphysicsC.F90: computing GM skewsion w/ streamfunction computed by boundary value problem. [Note] ocean_nphysicsC.F90: neutral_physics_limit=.true. Will revert to horizontal diffusion for points where tracer is outside specified range. [Note] ocean_nphysicsC.F90: dm_taper=.true. Will use the tanh scheme of Danabasoglu and McWilliams to taper neutral diffusion in steep sloped regions flux dom neutral domain decomposition whalo = 1, ehalo = 1, shalo = 1, nhalo = 1 X-AXIS = 23 23 23 23 22 22 22 22 22 22 22 22 23 23 23 23 Y-AXIS = 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 NOTE from PE 0: mpp_domains_define.inc(mpp_define_io_domain): io domain will not be defined for flux dom neutral when one or both entry of io_layout is not positive [Note] ocean_nphysics_util.F90: Starting ocean_nphysics_util fields from raw initialization. aredi_equal_agm=.false. and agm_read_restart=.false. => aredi_array set to static profiles. [Note] ocean_nphysics_util.F90: aredi_equal_agm=.false. allows aredi_array to differ from agm_array ---Neutral direction slope check I for linear stability of neutral diffusion--- With a neutral physics time step (secs) of 0.3600000E+04 the most stringent linear stability constraint was found at the following ocean cell: long( 201, 246) = -0.7950085E+02 lat ( 201, 246) = 0.6508043E+02 thick( 201, 246, 5) = 0.5285632E+01 aredi( 201, 246, 5) = 0.6000000E+03 delta_iso = 0.2215947E-01 is the maximum neutral direction slope available for linear stability of the neutral diffusion scheme. The namelist parameter smax should conservatively be <= delta_iso. ---Neutral direction slope check II for linear stability of neutral diffusion--- Assuming maximum Redi neutral diffusion slope of 0.1000000E-01 and neutral physics time step (secs) of 0.3600000E+04 the most stringent linear stability constraint was found at the following ocean cell: long( 201, 246) = -0.7950085E+02 lat ( 201, 246) = 0.6508043E+02 thick( 201, 246, 5)= 0.5285632E+01 A_max = 0.1317569E+04 (m^2/sec) is the maximum neutral diffusivity available for linear stability of the neutral diffusion scheme. Conservatively, neutral diffusivities used in the model should be less than A_max. -------------------------------------------------------------------------------- &OCEAN_NPHYSICS_NEW_NML USE_THIS_MODULE = F, DRHODZ_SMOOTH_VERT = F, DRHODZ_SMOOTH_HORZ = F, SMAX = 1.000000000000000E-002, VEL_MICOM_SMOOTH = 0.200000000000000 / &OCEAN_NPHYSICS_UTIL_NEW_NML NUM_121_PASSES = 1 / [Note] ocean_nphysics_new.F90: NOT using ocean_nphysics_new. &OCEAN_SUBMESOSCALE_NML USE_THIS_MODULE = T, DEBUG_THIS_MODULE = F, DIAG_STEP = 1200, USE_HBLT_CONSTANT = F, USE_HBLT_EQUAL_MLD = T, SMOOTH_HBLT = F, SMOOTH_HBLT_NUM = 2, CONSTANT_HBLT = 100.000000000000 , COEFFICIENT_CE = 7.000000000000001E-002, TIME_CONSTANT = 86400.0000000000 , FRONT_LENGTH_CONST = 5000.00000000000 , MIN_KBLT = 4, MINIMUM_HBLT = 0.000000000000000E+000, SMOOTH_PSI = T, SMOOTH_PSI_NUM = 2, FRONT_LENGTH_DEFORM_RADIUS = T, LIMIT_PSI = T, USE_PSI_LEGACY = F, LIMIT_PSI_VELOCITY_SCALE = 0.500000000000000 , SUBMESO_LIMIT_FLUX = T, SMOOTH_ADVECT_TRANSPORT = T, SMOOTH_ADVECT_TRANSPORT_NUM = 2, SUBMESO_SKEW_FLUX = T, SUBMESO_ADVECT_FLUX = F, SUBMESO_ADVECT_UPWIND = T, SUBMESO_ADVECT_SWEBY = F, SUBMESO_ADVECT_LIMIT = F, SUBMESO_ADVECT_ZERO_BDY = F, SUBMESO_DIFFUSION = F, SUBMESO_DIFFUSION_SCALE = 1.00000000000000 , SUBMESO_DIFFUSION_BIHARMONIC = F / NOTE from PE 0: ==>Note: USING ocean_submesoscale_mod ==>Note: For ocean_submesoscale, setting bldepth equal to diagnosed mld. ==>Note: For ocean_submesoscale, tendency computed as skew flux convergence. mdfl domain decomposition whalo = 2, ehalo = 2, shalo = 2, nhalo = 2 X-AXIS = 23 23 23 23 22 22 22 22 22 22 22 22 23 23 23 23 Y-AXIS = 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 NOTE from PE 0: mpp_domains_define.inc(mpp_define_io_domain): io domain will not be defined for mdfl when one or both entry of io_layout is not positive flux dom submeso domain decomposition whalo = 1, ehalo = 1, shalo = 1, nhalo = 1 X-AXIS = 23 23 23 23 22 22 22 22 22 22 22 22 23 23 23 23 Y-AXIS = 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 NOTE from PE 0: mpp_domains_define.inc(mpp_define_io_domain): io domain will not be defined for flux dom submeso when one or both entry of io_layout is not positive &OCEAN_LAP_FRICTION_NML LAP_FRICTION_SCHEME = general , DEBUG_THIS_MODULE = F, WRITE_A_RESTART = T / ==>Note from ocean_lap_friction_init: general laplacian friction scheme for B-grid is used. &OCEAN_LAPGEN_FRICTION_NML USE_THIS_MODULE = T, DEBUG_THIS_MODULE = F, BOTTOM_5POINT = T, K_SMAG_ISO = 0.000000000000000E+000, K_SMAG_ANISO = 0.000000000000000E+000, VEL_MICOM_ISO = 0.100000000000000 , VEL_MICOM_ANISO = 0.000000000000000E+000, EQ_VEL_MICOM_ISO = 0.000000000000000E+000, EQ_VEL_MICOM_ANISO = 0.000000000000000E+000, EQ_LAT_MICOM = 0.000000000000000E+000, EQUATORIAL_ZONAL = F, EQUATORIAL_ZONAL_LAT = 0.000000000000000E+000, EQUATORIAL_NO_SMAG = F, VISCOSITY_NCAR = T, VISCOSITY_NCAR_2000 = F, VISCOSITY_NCAR_2007 = T, NCAR_ISOTROPIC_OFF_EQUATOR = F, NCAR_ONLY_EQUATORIAL = T, VCONST_1 = 8000000.00000000 , VCONST_2 = 0.000000000000000E+000, VCONST_3 = 0.800000000000000 , VCONST_4 = 5.000000000000000E-009, VCONST_5 = 3, VCONST_6 = 300000000.000000 , VCONST_7 = 100.000000000000 , VCONST_8 = 45.0000000000000 , DEBUG_NCAR_A = F, DEBUG_NCAR_B = F, VISC_VEL_SCALE_LENGTH = 150000.000000000 , NEPTUNE = F, NEPTUNE_LENGTH_EQ = 1200.00000000000 , NEPTUNE_LENGTH_POLE = 3000.00000000000 , NEPTUNE_DEPTH_MIN = 100.000000000000 , NEPTUNE_SMOOTH = T, NEPTUNE_SMOOTH_NUM = 1, RESTRICT_POLAR_VISC = T, RESTRICT_POLAR_VISC_LAT = 60.0000000000000 , RESTRICT_POLAR_VISC_RATIO = 0.350000000000000 , NCAR_ISOTROPIC_AT_DEPTH = F, NCAR_ISOTROPIC_DEPTH = 4000.00000000000 , NCAR_ISOTROPIC_AT_DEPTH_VISC = 10000.0000000000 , DIVERGENCE_DAMP = F, DIVERGENCE_DAMP_VEL_MICOM = 0.000000000000000E+000, VISCOSITY_SCALE_BY_ROSSBY = T, VISCOSITY_SCALE_BY_ROSSBY_POWER = 4.00000000000000 , ASYNC_DOMAIN_UPDATE = F, BLOCKSIZE = 10, USE_SIDE_DRAG_FRICTION = F, SIDE_DRAG_FRICTION_SCALING = 1.00000000000000 , SIDE_DRAG_FRICTION_UVMAG_MAX = 10.0000000000000 , SIDE_DRAG_FRICTION_MAX = 1.00000000000000 / NOTE from PE 0: ==> NOTE: USING ocean_lapgen_friction_mod. ==>Note: not using asynchronous domain update in the vertical loop. This may be slow. ==> Note from ocean_lapgen_friction_mod: using forward time step of (secs) 3600.00 ==> Note: Scaling the laplacian viscosity according to grid scale and Rossby radius. ==> Note: Will reduce horizontal friction to a 5point Laplacian on the bottom This helps to alleviate numerical problems with thin bottom partial cells. ==> NOTE: USING background horz viscosities according to NCAR CCSM2.0 algorithm. ==> NOTE: USING NCAR viscosity as formulated in 2007. NCAR vconst_1 (cm^2/sec) = 0.8000E+07 NCAR vconst_2 = 0.000000000000000E+000 NCAR vconst_3 = 0.800000000000000 NCAR vconst_4 (1/cm) = 5.000000000000000E-009 NCAR vconst_5 = 3 NCAR vconst_6 (cm^2/sec) = 0.3000E+09 NCAR vconst_7 (cm/sec) = 100.000000000000 NCAR vconst_8 (degrees) = 45.0000000000000 ==>ncar_only_equatorial=.true. =>ncar scheme only in band +/- lat 0.0000 ==> NOTE: Setting horz isotropic Smagorinsky viscosity to zero. ==> NOTE: Setting horz anisotropic Smagorinsky viscosity to zero. Using restrict_polar_visc to lower visc_crit poleward of (deg) 60.00000 by an amount given by the fraction 0.35000 This approach is useful when coupling to ice, where effective (ocn+ice) visc > ocn visc. &OCEAN_BIH_FRICTION_NML BIH_FRICTION_SCHEME = general , DEBUG_THIS_MODULE = F, WRITE_A_RESTART = T / ==>Note from ocean_bih_friction_init: general biharmonic friction scheme for B-grid is used. &OCEAN_BIHGEN_FRICTION_NML USE_THIS_MODULE = T, DEBUG_THIS_MODULE = F, K_SMAG_ISO = 2.00000000000000 , K_SMAG_ANISO = 0.000000000000000E+000, VEL_MICOM_ISO = 4.000000000000000E-002, VEL_MICOM_ANISO = 0.000000000000000E+000, EQ_VEL_MICOM_ISO = 0.000000000000000E+000, EQ_VEL_MICOM_ANISO = 0.000000000000000E+000, EQ_LAT_MICOM = 0.000000000000000E+000, VEL_MICOM_BOTTOM = 1.000000000000000E-002, BOTTOM_5POINT = T, EQUATORIAL_ZONAL = F, EQUATORIAL_ZONAL_LAT = 0.000000000000000E+000, VISC_CRIT_SCALE = 0.250000000000000 , READ_AISO_BIH_BACK = F, NCAR_BOUNDARY_SCALING = T, NCAR_RESCALE_POWER = 2, NCAR_VCONST_4 = 2.000000000000000E-008, NCAR_VCONST_5 = 5, NCAR_BOUNDARY_SCALING_READ = F, NEPTUNE = F, NEPTUNE_LENGTH_EQ = 4200.00000000000 , NEPTUNE_LENGTH_POLE = 17000.0000000000 , NEPTUNE_DEPTH_MIN = 100.000000000000 , NEPTUNE_SCALING = 1.00000000000000 , NEPTUNE_SMOOTH = T, NEPTUNE_SMOOTH_NUM = 1, VISC_DIVERGE_SCALING = 0.000000000000000E+000, USE_SIDE_DRAG_FRICTION = F, SIDE_DRAG_FRICTION_SCALING = 1.00000000000000 , SIDE_DRAG_FRICTION_UVMAG_MAX = 10.0000000000000 , SIDE_DRAG_FRICTION_MAX = 1.00000000000000 / NOTE from PE 0: ==> NOTE: USING ocean_bihgen_friction_mod. ==> Note from ocean_bihgen_friction_mod: using forward time step of (secs) 3600.00 ==> NOTE: Will make horizontal friction to a 5point Laplacian on the bottom This helps alleviate numerical problems with thin bottom partial cells. Computing horziontal isotropic biharmonic viscosity via Smagorinsky. Setting horzizontal anisotropic biharmonic Smagorinsky viscosity to zero. Computing background horzizontal biharmonic isotropic viscosity via MICOM. Setting background horziontal biharmonic anisotropic viscosity to zero. Note: rescaling background bih viscosities so they are larger in western boundaries. From ncar_boundary_scale, minimum ncar_rescale = 0.100000E+01 &OCEAN_MOMENTUM_SOURCE_NML VERBOSE_INIT = T, USE_THIS_MODULE = T, DEBUG_THIS_MODULE = F, USE_RAYLEIGH_DAMP_TABLE = T, RAYLEIGH_DAMP_EXP_FROM_BOTTOM = F, RAYLEIGH_DAMP_EXP_SCALE = 100.000000000000 , RAYLEIGH_DAMP_EXP_TIME = 864000.000000000 / ==>Note from ocean_momentum_source_mod: USING this module ==>Note: ocean_momentum_source_init will read Rayleigh damping coefficients fro m rayleigh_damp_table. &OCEAN_FORM_DRAG_NML VERBOSE_INIT = T, USE_THIS_MODULE = F, DEBUG_THIS_MODULE = F, USE_FORM_DRAG_AIKI = F, CPRIME_AIKI = 0.600000000000000 , FORM_DRAG_AIKI_BOTTOM_LAYER = F, FORM_DRAG_AIKI_BOTTOM_KLEVELS = 3, FORM_DRAG_AIKI_SCALE_BY_GRADH = F, FORM_DRAG_AIKI_GRADH_MAX = 5.000000000000000E-002, FORM_DRAG_AIKI_GRADH_POWER = 1.00000000000000 , FORM_DRAG_AIKI_SCALE_BY_GM = F, USE_FORM_DRAG_GBATCH = F, VISC_CBU_FORM_DRAG_MAX = 1.00000000000000 , VEL_FORM_DRAG_MAX = 1.00000000000000 , N_SQUARED_MIN = 1.000000000000000E-010, AGM_FORM_DRAG = 600.000000000000 , FORM_DRAG_GBATCH_SURF_LAYER = F, KSURF_BLAYER_MIN = 3, FORM_DRAG_GBATCH_ALPHA_F2 = F, FORM_DRAG_GBATCH_ALPHA = 300000000.000000 , FORM_DRAG_GBATCH_F2OVERN2 = F, FORM_DRAG_GBATCH_F2OVERNB2 = F, FORM_DRAG_GBATCH_SMOOTH_N2 = F, NUM_121_PASSES = 1, FORM_DRAG_GBATCH_F2OVERNO2 = F, FORM_DRAG_GBATCH_NO = 5.000000000000000E-003 / NOTE from PE 0: ==>Note from ocean_form_drag_mod: NOT USING this module &OCEAN_TRACER_ADVECT_NML DEBUG_THIS_MODULE = F, LIMIT_WITH_UPWIND = F, ADVECT_SWEBY_ALL = T, ZERO_TRACER_ADVECT_HORZ = F, ZERO_TRACER_ADVECT_VERT = F, WRITE_A_RESTART = T, PSOM_LIMIT_PRATHER = F, READ_BASIN_MASK = F, ASYNC_DOMAIN_UPDATE = T / ==>Note: using asynchrnous domain update for MDFL SWEBY_all ==>ocean_tracer_advect_mod: advect_sweby_all=.true. so all tracers advected with mdfl_sweby, regardless the settings in field_table. This method exploits mpp_update_domain capabilities and is faster in some cases. flux domain decomposition whalo = 1, ehalo = 1, shalo = 1, nhalo = 1 X-AXIS = 23 23 23 23 22 22 22 22 22 22 22 22 23 23 23 23 Y-AXIS = 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 fourth domain decomposition whalo = 2, ehalo = 2, shalo = 2, nhalo = 2 X-AXIS = 23 23 23 23 22 22 22 22 22 22 22 22 23 23 23 23 Y-AXIS = 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 NOTE from PE 0: mpp_domains_define.inc(mpp_define_io_domain): io domain will not be defined for fourth when one or both entry of io_layout is not positive sixth domain decomposition whalo = 3, ehalo = 3, shalo = 3, nhalo = 3 X-AXIS = 23 23 23 23 22 22 22 22 22 22 22 22 23 23 23 23 Y-AXIS = 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 NOTE from PE 0: mpp_domains_define.inc(mpp_define_io_domain): io domain will not be defined for sixth when one or both entry of io_layout is not positive quicker domain decomposition whalo = 2, ehalo = 2, shalo = 2, nhalo = 2 X-AXIS = 23 23 23 23 22 22 22 22 22 22 22 22 23 23 23 23 Y-AXIS = 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 NOTE from PE 0: mpp_domains_define.inc(mpp_define_io_domain): io domain will not be defined for quicker when one or both entry of io_layout is not positive mdfl domain decomposition whalo = 2, ehalo = 2, shalo = 2, nhalo = 2 X-AXIS = 23 23 23 23 22 22 22 22 22 22 22 22 23 23 23 23 Y-AXIS = 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 NOTE from PE 0: mpp_domains_define.inc(mpp_define_io_domain): io domain will not be defined for mdfl when one or both entry of io_layout is not positive mdppm domain decomposition whalo = 4, ehalo = 4, shalo = 4, nhalo = 4 X-AXIS = 23 23 23 23 22 22 22 22 22 22 22 22 23 23 23 23 Y-AXIS = 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 NOTE from PE 0: mpp_domains_define.inc(mpp_define_io_domain): io domain will not be defined for mdppm when one or both entry of io_layout is not positive mdmdt domain decomposition whalo = 4, ehalo = 4, shalo = 4, nhalo = 4 X-AXIS = 23 23 23 23 22 22 22 22 22 22 22 22 23 23 23 23 Y-AXIS = 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 NOTE from PE 0: mpp_domains_define.inc(mpp_define_io_domain): io domain will not be defined for mdmdt when one or both entry of io_layout is not positive &OCEAN_VELOCITY_ADVECT_NML DEBUG_THIS_MODULE = F, ZERO_VELOCITY_ADVECT_HORZ = F, ZERO_VELOCITY_ADVECT_VERT = F, VELOCITY_ADVECT_CENTERED = T, VELOCITY_ADVECT_UPWIND = F / ==>Note: running MOM with traditional second order centred advection of linear momentum. &OCEAN_CONVECT_NML USE_THIS_MODULE = F, CONVECT_NCON = F, NCON = 7, CONVECT_FULL_SCALAR = F, CONVECT_FULL_VECTOR = T / ==>Note: NOT using convective adjustment in gravitationally unstable water columns. &OCEAN_SBC_NML TEMP_RESTORE_TSCALE = -1.00000000000000 , SALT_RESTORE_TSCALE = 15.0000000000000 , SALT_RESTORE_UNDER_ICE = T, SALT_RESTORE_AS_SALT_FLUX = T, ETA_RESTORE_TSCALE = -30.0000000000000 , ZERO_NET_PME_ETA_RESTORE = F, ROTATE_WINDS = F, TAUX_SINX = F, TAUY_SINY = F, USE_WATERFLUX = T, WATERFLUX_TAVG = F, MAX_ICE_THICKNESS = 8.00000000000000 , RUNOFFSPREAD = F, CALVINGSPREAD = F, USE_WATERFLUX_OVERRIDE_CALVING = F, USE_WATERFLUX_OVERRIDE_EVAP = F, USE_WATERFLUX_OVERRIDE_FPREC = F, SALINITY_REF = 35.0000000000000 , ZERO_NET_SALT_RESTORE = T, ZERO_NET_WATER_RESTORE = T, ZERO_NET_WATER_COUPLER = T, ZERO_NET_WATER_COUPLE_RESTORE = T, ZERO_NET_SALT_CORRECTION = F, ZERO_NET_WATER_CORRECTION = F, DEBUG_WATER_FLUXES = F, ZERO_WATER_FLUXES = F, ZERO_CALVING_FLUXES = F, ZERO_PME_FLUXES = F, ZERO_RUNOFF_FLUXES = F, ZERO_RIVER_FLUXES = F, CONVERT_RIVER_TO_PME = F, ZERO_HEAT_FLUXES = F, ZERO_SURFACE_STRESS = F, AVG_SFC_VELOCITY = T, AVG_SFC_TEMP_SALT_ETA = T, ICE_SALT_CONCENTRATION = 4.000000000000000E-003, RUNOFF_SALINITY = 0.000000000000000E+000, RUNOFF_TEMP_MIN = 0.000000000000000E+000, READ_RESTORE_MASK = F, RESTORE_MASK_GFDL = F, LAND_MODEL_HEAT_FLUXES = F, USE_FULL_PATM_FOR_SEA_LEVEL = F, MAX_DELTA_SALINITY_RESTORE = 0.500000000000000 , DO_FLUX_CORRECTION = F, TEMP_CORRECTION_SCALE = 0.000000000000000E+000, SALT_CORRECTION_SCALE = 0.000000000000000E+000, TAU_X_CORRECTION_SCALE = 0.000000000000000E+000, TAU_Y_CORRECTION_SCALE = 0.000000000000000E+000, DO_BITWISE_EXACT_SUM = T, SBC_HEAT_FLUXES_CONST = F, SBC_HEAT_FLUXES_CONST_VALUE = 0.000000000000000E+000, SBC_HEAT_FLUXES_CONST_SEASONAL = F, USE_CONSTANT_SSS_FOR_RESTORE = F, CONSTANT_SSS_FOR_RESTORE = 35.0000000000000 , USE_CONSTANT_SST_FOR_RESTORE = F, CONSTANT_SST_FOR_RESTORE = 12.0000000000000 , USE_IDEAL_CALVING = F, USE_IDEAL_RUNOFF = F, CONSTANT_HLF = T, CONSTANT_HLV = T, READ_STOKES_DRIFT = F, DO_LANGMUIR = F / &OCEAN_SBC_OFAM_NML RESTORE_MASK_OFAM = F, RIVER_TEMP_OFAM = F / sbc domain decomposition whalo = 0, ehalo = 0, shalo = 0, nhalo = 0 X-AXIS = 23 23 23 23 22 22 22 22 22 22 22 22 23 23 23 23 Y-AXIS = 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 NOTE from PE 0: mpp_domains_define.inc(mpp_define_io_domain): io domain will not be defined for sbc when one or both entry of io_layout is not positive WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 ==>Note from ocean_sbc_mod: applying surface restoring to temp WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 ==>Note from ocean_sbc_mod: applying surface restoring to salt ==>Note from ocean_sbc_mod: if inputting river water, enable rivermix_mod to get river tracers into ocean. ==>Note from ocean_sbc_mod: temp_restore_tscale < 0. no surface restoring for t emp ==>Note from ocean_sbc_mod: salt_restore_under_ice=.true. => sss restore even u nder ice. ==>Note from ocean_sbc_mod: zero_net_water_restore=.true.=>zero net restoring w ater put in ocean. ==>Note from ocean_sbc_mod: zero_net_water_correction=.false.=>nonzero net corr ection water put in ocean. ==>Note from ocean_sbc_mod: zero_net_water_coupler=.true.=>zero water into ocea n via coupler (sans the sea ice). ==>ocean_sbc_mod: zero_net_water_couple_restore=.true.=>zero water into ocean f rom restore + coupler (sans the sea ice). ==>Note from ocean_sbc_mod: eta_restore_tscale < 0. no surface restoring for et a ==>If coupling, then avg_sfc_velocity=.true. means will pass averaged ocean vel ocity to ice model. ==>If coupling, then avg_sfc_temp_salt_eta=.true. means will pass averaged sst, sss, eta to ice model. ==>Note from ocean_sbc_mod: Using constant latent heat of fusion at ocean surfa ce. ==>Note from ocean_sbc_mod: Using constant latent heat of evaporation at ocean surface. ==>Note that diagnose_sea_level_forcing==.false., so no "eta_tend_" fields will be diagnosed. &OCEAN_BBC_NML BMF_IMPLICIT = F, CDBOT = 1.000000000000000E-003, URESIDUAL = 5.000000000000000E-002, CDBOT_LAW_OF_WALL = F, LAW_OF_WALL_ROUGH_LENGTH = 1.000000000000000E-002, CDBOT_ROUGHNESS_LENGTH = F, USE_GEOTHERMAL_HEATING = F, CONVERT_GEOTHERMAL = 1.000000000000000E-003, CDBOT_HI = 3.000000000000000E-003, CDBOT_LO = 1.000000000000000E-003, CDBOT_GAMMA = 40.0000000000000 , UVMAG_MAX = 10.0000000000000 , BMF_MAX = 1.00000000000000 , DEBUG_THIS_MODULE = F, CDBOT_ROUGHNESS_UAMP = F, CDBOT_HH = 1100.00000000000 , CDBOT_UU = 1.00000000000000 , CDBOT_WAVE = F / &OCEAN_BBC_OFAM_NML READ_TIDE_SPEED = F, URESIDUAL2_MAX = 1.00000000000000 / ==>Note: NOT reading tide_speed for ocean_vert_tidal_mod. NOTE from PE 0: ==>ocean_vert_tidal_mod: Setting tide_speed to default value. &OCEAN_SHORTWAVE_NML USE_THIS_MODULE = T, USE_SHORTWAVE_GFDL = F, USE_SHORTWAVE_CSIRO = T, USE_SHORTWAVE_JERLOV = F, USE_SHORTWAVE_EXT = F / NOTE from PE 0: ==>Note: USING shortwave_mod. &OCEAN_SHORTWAVE_CSIRO_NML USE_THIS_MODULE = T, READ_DEPTH = T, DEPTH_DEFAULT = 20.0000000000000 , ZMAX_PEN = 7000.00000000000 , SW_FRAC_TOP = 0.000000000000000E+000, DEBUG_THIS_MODULE = F, ENFORCE_SW_FRAC = T, SW_PEN_FIXED_DEPTHS = F / NOTE from PE 0: ==>Note: USING shortwave_csiro_mod. NOTE from PE 0: ==>Note: Reading in attenuation length scale from data file for shortwave penetration. WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 WARNING from PE 0: set_date_c: Year zero is invalid. Resetting year to 1 =>Note: computing solar shortwave penetration. Assume stf has sw-radiation fiel d included. Hence, solar shortwave penetration effects placed in sw_source wil l subtract out the effects of shortwave at k=1 to avoid double-counting. =>Note: enforce_sw_frac=.true. enforcing monotonic decrease of sw_frac with dep th. &OCEAN_SPONGES_TRACER_NML USE_THIS_MODULE = F, DAMP_COEFF_3D = F / &OCEAN_SPONGES_TRACER_OFAM_NML USE_ADAPTIVE_RESTORE = F, USE_SPONGE_AFTER_INIT = F, USE_NORMALISING = F, USE_HARD_THUMP = F, ATHRESH = 0.500000000000000 , TAUMIN = 720.000000000000 , LAMBDA = 8.300000000000000E-003, NPOWER = 1.00000000000000 , DAYS_TO_RESTORE = 1, SECS_TO_RESTORE = 0, DEFLATE = F, DEFLATE_FRACTION = 0.600000000000000 , LIMIT_TEMP = F, LIMIT_TEMP_MIN = -1.80000000000000 , LIMIT_TEMP_RESTORE = 10800.0000000000 , LIMIT_SALT = F, LIMIT_SALT_MIN = 1.000000000000000E-002, LIMIT_SALT_RESTORE = 3600.00000000000 / ==>Note from ocean_sponges_tracer_mod: NOT using ocean tracer sponges. &OCEAN_SPONGES_VELOCITY_NML USE_THIS_MODULE = F, DAMP_COEFF_3D = F / &OCEAN_SPONGES_VELOCITY_OFAM_NML USE_ADAPTIVE_RESTORE = F, USE_SPONGE_AFTER_INIT = F, USE_NORMALISING = F, USE_HARD_THUMP = F, ATHRESH = 0.500000000000000 , TAUMIN = 720.000000000000 , LAMBDA = 8.300000000000000E-003, NPOWER = 1.00000000000000 , DAYS_TO_RESTORE = 1, SECS_TO_RESTORE = 0 / ==>Note from ocean_sponges_velocity_mod: NOT using this module: no velocity spo nges. &OCEAN_SPONGES_ETA_NML USE_THIS_MODULE = F / &OCEAN_SPONGES_ETA_OFAM_NML USE_ADAPTIVE_RESTORE = F, USE_SPONGE_AFTER_INIT = F, USE_NORMALISING = F, USE_HARD_THUMP = F, ATHRESH = 0.500000000000000 , TAUMIN = 720.000000000000 , LAMBDA = 8.300000000000000E-003, NPOWER = 1.00000000000000 , DAYS_TO_RESTORE = 1, SECS_TO_RESTORE = 0 / ==>Note from ocean_sponges_eta_mod: NOT using this module. ==>Warning: ocean_xlandinsert_init found n < 1 for xland_insert table. Will NO T use ocean_xlandinsert. ==>Warning: ocean_riverspread_init: n<1 for riverspread table. Will NOT use tab le for ocean_riverspread. &OCEAN_RIVERSPREAD_NML USE_THIS_MODULE = T, DEBUG_THIS_MODULE = F, RIVERSPREAD_DIFFUSION = F, RIVERSPREAD_DIFFUSION_PASSES = 0, VEL_MICOM_SMOOTH = 0.200000000000000 / NOTE from PE 0: ==>From ocean_riverspread_mod: Using riverspread module to mix river water into the ocean. &OCEAN_RIVERMIX_NML USE_THIS_MODULE = T, DEBUG_THIS_MODULE = F, DEBUG_ALL_IN_TOP_CELL = F, DEBUG_THIS_MODULE_HEAT = F, RIVER_DIFFUSE_TEMP = F, RIVER_DIFFUSE_SALT = F, RIVER_DIFFUSION_THICKNESS = 0.000000000000000E+000, RIVER_DIFFUSIVITY = 0.000000000000000E+000, DISCHARGE_COMBINE_RUNOFF_CALVE = T, RIVER_INSERTION_THICKNESS = 40.0000000000000 , RUNOFF_INSERTION_THICKNESS = 0.000000000000000E+000, CALVING_INSERTION_THICKNESS = 0.000000000000000E+000, DO_BITWISE_EXACT_SUM = F / NOTE from PE 0: ==>From ocean_rivermix_mod: Using rivermix module to mix liquid and/or solid runoff into the ocean. ==>Note: discharging calving+runoff together. The alternative is to separately discharge. ==>Note: if using waterflux and rivers, then will discharge river tracer over 4 grid points in vertical &OCEAN_OVEREXCHANGE_NML USE_THIS_MODULE = F, DEBUG_THIS_MODULE = F, OVEREXCH_NPTS = 4, OVEREXCH_WIDTH = 1, OVEREXCH_WEIGHT_FAR = F, OVERFLOW_MU = 1.000000000000000E-004, OVERFLOW_DELTA = 0.333300000000000 , OVERFLOW_UMAX = 5.00000000000000 , DO_BITWISE_EXACT_SUM = F, OVEREXCH_STABILITY = 0.250000000000000 , OVEREXCH_MIN_THICKNESS = 4.00000000000000 , OVEREXCH_CHECK_EXTREMA = F / NOTE from PE 0: ==>From ocean_overexchange_mod: NOT using overflow exchange scheme. &OCEAN_MIXDOWNSLOPE_NML USE_THIS_MODULE = T, DEBUG_THIS_MODULE = F, MIXDOWNSLOPE_NPTS = 4, MIXDOWNSLOPE_WIDTH = 1, MIXDOWNSLOPE_WEIGHT_FAR = F, MIXDOWNSLOPE_FRAC_CENTRAL = 0.250000000000000 , DO_BITWISE_EXACT_SUM = F, READ_MIXDOWNSLOPE_MASK = F, MIXDOWNSLOPE_MASK_GFDL = F / NOTE from PE 0: ==>From ocean_mixdownslope_mod: USING downslope mixing scheme. In ocean_mixdownslope_mod: mixdownslope_npts = 4 Be sure this number is smaller than dimensions of computational domain. mixdownslope domain decomposition whalo = 4, ehalo = 4, shalo = 4, nhalo = 4 X-AXIS = 23 23 23 23 22 22 22 22 22 22 22 22 23 23 23 23 Y-AXIS = 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 NOTE from PE 0: mpp_domains_define.inc(mpp_define_io_domain): io domain will not be defined for mixdownslope when one or both entry of io_layout is not positive &OCEAN_OVERFLOW_NML USE_THIS_MODULE = F, DEBUG_THIS_MODULE = F, OVERFLOW_MU = 1.000000000000000E-004, OVERFLOW_DELTA = 0.333300000000000 , OVERFLOW_UMAX = 1.000000000000000E-002, DO_BITWISE_EXACT_SUM = F, NO_RETURN_FLOW = F, TRANSPORT_UNITS = Sv / NOTE from PE 0: ==>From ocean_overflow_mod: NOT using Campin and Goosse overflow scheme. ==>Warning: ocean_overflow_OFP_init found n_src < 1 for overflow_OFP table. Will NOT use ocean_overflow_OFP. ==>Note from fm_util_mod(fm_util_start_namelist)[ocean_age_tracer_mod(ocean_age _tracer_start)]: Processing namelist ocean_age_tracer/global ==>Note from ocean_age_tracer_mod(ocean_age_tracer_start): Assigning month 1 ==>Note from ocean_age_tracer_mod(set_array): age_global region: 1 ==>Note from ocean_age_tracer_mod(ocean_age_tracer_start): Duplicating month 1 as 2 ==>Note from ocean_age_tracer_mod(ocean_age_tracer_start): Duplicating month 1 as 3 ==>Note from ocean_age_tracer_mod(ocean_age_tracer_start): Duplicating month 1 as 4 ==>Note from ocean_age_tracer_mod(ocean_age_tracer_start): Duplicating month 1 as 5 ==>Note from ocean_age_tracer_mod(ocean_age_tracer_start): Duplicating month 1 as 6 ==>Note from ocean_age_tracer_mod(ocean_age_tracer_start): Duplicating month 1 as 7 ==>Note from ocean_age_tracer_mod(ocean_age_tracer_start): Duplicating month 1 as 8 ==>Note from ocean_age_tracer_mod(ocean_age_tracer_start): Duplicating month 1 as 9 ==>Note from ocean_age_tracer_mod(ocean_age_tracer_start): Duplicating month 1 as 10 ==>Note from ocean_age_tracer_mod(ocean_age_tracer_start): Duplicating month 1 as 11 ==>Note from ocean_age_tracer_mod(ocean_age_tracer_start): Duplicating month 1 as 12 &OCEAN_ADV_VEL_DIAG_NML MAX_CFL_VALUE = 100.000000000000 , LARGE_CFL_VALUE = 10.0000000000000 , VERBOSE_CFL = F, DIAG_STEP = 4320 / ==>Maximum T-->U remapping error = 6.049E-05 m/s at (i,j) = ( 199, 246), (lon,lat) = ( -81.00, 65.15) ==>Note: T-->U remapping error will be small (i.e., order 1e-20) only for spherical grids. &OCEAN_TRACER_DIAG_NML TRACER_CONSERVE_DAYS = 1.00000000000000 , DIAG_STEP = 48, PSU2PPT = 1.00486700000000 , DEBUG_DIAGNOSE_MIXINGA = F, DEBUG_DIAGNOSE_MIXINGB = F, DEBUG_DIAGNOSE_MIXINGC = F, DEBUG_DIAGNOSE_MIXINGD = F, SMOOTH_KAPPA_SORT = 0, RHO_GRAD_MIN = 1.000000000000000E-005, RHO_GRAD_MAX = 1.000000000000000E+028, BUOYANCY_CRIT = 3.000000000000000E-004, DO_BITWISE_EXACT_SUM = F, FRAZIL_FACTOR = 1.00000000000000 , SMOOTH_MLD = F, SMOOTH_MLD_FOR_SUBDUCTION = T, DTHETA_CRIT = 2.00000000000000 / Note: tracer and mass/volume conservation tests based on time_tendency==twolevel. Note: Set frazil_factor = 1.00 for computation of heat diagnostics. Be sure this agrees with the value set in nml for ocean_frazil_mod &OCEAN_VELOCITY_DIAG_NML DIAG_STEP = 4320, ENERGY_DIAG_STEP = 4320, DO_BITWISE_EXACT_SUM = F, DEBUG_THIS_MODULE = F, MAX_CFL_VALUE = 100.000000000000 , LARGE_CFL_VALUE = 10.0000000000000 , VERBOSE_CFL = F, LAND_CELL_NUM_MAX = 100 / &OCEAN_INCREMENT_ETA_NML USE_THIS_MODULE = F, FRACTION_INCREMENT = 1.00000000000000 , DAYS_TO_INCREMENT = 0, SECS_TO_INCREMENT = 1800 / &OCEAN_INCREMENT_TRACER_NML USE_THIS_MODULE = F, FRACTION_INCREMENT = 1.00000000000000 , DAYS_TO_INCREMENT = 0, SECS_TO_INCREMENT = 1800 / &OCEAN_INCREMENT_VELOCITY_NML USE_THIS_MODULE = F, FRACTION_INCREMENT = 1.00000000000000 , DAYS_TO_INCREMENT = 0, SECS_TO_INCREMENT = 1800 / &OCEAN_WAVE_NML WAVEDAMP = -10.0000000000000 , DAMP_WHERE_ICE = T, WRITE_A_RESTART = T, DEBUG_THIS_MODULE = F, USE_TMA = T, FILTER_WAVE_MOM = T, USE_THIS_MODULE = F / ==>Note: Not using the idealized ocean surface wave module. auscom_ice_nml= &AUSCOM_ICE_NML DT_CPL = 3600, TLTHK0 = 10.0000000000000 , POP_ICEDIAG = T, DO_ICE_ONCE = F, KMXICE = 5, FIXMELTT = F, TMELT = -0.216000000000000 , LIMIT_SRFSTRESS = F, MSTRESS = 2.00000000000000 , USE_IOAICE = T, AICE_CUTOFF = 0.150000000000000 , ICEMLT_FACTOR = 1.00000000000000 , FRAZIL_FACTOR = 1.00000000000000 , ICEFORM_ADJ_SALT = F, SIGN_STFLX = 1.00000000000000 , REDSEA_GULFBAY_SFIX = F, IRS1 = 314, IRE1 = 324, JRS1 = 169, JRE1 = 196, IRS2 = 325, IRE2 = 331, JRS2 = 169, JRE2 = 180, IGS = 328, IGE = 345, JGS = 189, JGE = 198, KSMAX = 5, SFIX_HOURS = 12, CHK_I2O_FIELDS = F, CHK_O2I_FIELDS = F, CHK_FIELDS_PERIOD = 1, CHK_FIELDS_START_TIME = 0 / &OCEAN_DRIFTERS_NML USE_THIS_MODULE = F, OUTPUT_INTERVAL = 1 / ======== COMPLETED MOM INITIALIZATION ======== MOM: (init_cpl), my_task opened log file: 20 oceout000105 MOM: (init_cpl), my_task opened log file: 239 oceout000324 MOM: (init_cpl), my_task opened log file: 161 oceout000246 MOM: (init_cpl), my_task opened log file: 32 oceout000117 &MOM_OASIS3_INTERFACE_NML NUM_FIELDS_IN = 15, NUM_FIELDS_OUT = 7, FIELDS_IN = u_flux v_flux lprec fprec salt_flxmh_flux sw_flux q_flux t_flux lw_flux runof p aice wfimelt wfiform , FIELDS_OUT = t_surf s_surf u_surf v_surf dssldx dssldy frazil , SEND_BEFORE_OCEAN_UPDATE = F, SEND_AFTER_OCEAN_UPDATE = T / MOM: (init_cpl), my_task opened log file: 111 oceout000196 MOM: (init_cpl), my_task opened log file: 90 oceout000175 MOM: (init_cpl), my_task opened log file: 131 oceout000216 MOM: (init_cpl), my_task opened log file: 6 oceout000091 MOM: (init_cpl), my_task opened log file: 129 oceout000214 MOM: (init_cpl), my_task opened log file: 21 oceout000106 MOM: (init_cpl), my_task opened log file: 215 oceout000300 MOM: (init_cpl), my_task opened log file: 153 oceout000238 MOM: (init_cpl), my_task opened log file: 210 oceout000295 MOM: (init_cpl), my_task opened log file: 80 oceout000165 MOM: (init_cpl), my_task opened log file: 8 oceout000093 MOM: (init_cpl), my_task opened log file: 125 oceout000210 MOM: (init_cpl), my_task opened log file: 225 oceout000310 MOM: (init_cpl), my_task opened log file: 160 oceout000245 MOM: (init_cpl), my_task opened log file: 43 oceout000128 MOM: (init_cpl), my_task opened log file: 232 oceout000317 MOM: (init_cpl), my_task opened log file: 223 oceout000308 MOM: (init_cpl), my_task opened log file: 28 oceout000113 MOM: (init_cpl), my_task opened log file: 157 oceout000242 MOM: (init_cpl), my_task opened log file: 216 oceout000301 MOM: (init_cpl), my_task opened log file: 14 oceout000099 MOM: (init_cpl), my_task opened log file: 17 oceout000102 MOM: (init_cpl), my_task opened log file: 198 oceout000283 MOM: (init_cpl), my_task opened log file: 100 oceout000185 MOM: (init_cpl), my_task opened log file: 29 oceout000114 MOM: (init_cpl), my_task opened log file: 47 oceout000132 MOM: (init_cpl), my_task opened log file: 224 oceout000309 MOM: (init_cpl), my_task opened log file: 42 oceout000127 MOM: (init_cpl), my_task opened log file: 66 oceout000151 MOM: (init_cpl), my_task opened log 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CHK_O2I_FIELDS = F / &COUPLING_NML DT_CPL_AI = 10800, DT_CPL_IO = 3600, POP_ICEDIAG = T, USE_OCNSLOPE = F, USE_UMASK = F, ROTATE_WINDS = F, ICE_PRESSURE_ON = T, ICE_FWFLUX = T, LIMIT_ICEMELT = F, MELTLIMIT = -200.000000000000 , PRECIP_FACTOR = 1.00000000000000 , CST_OCN_ALBEDO = T, OCN_ALBEDO = 0.100000000000000 , GFDL_SURFACE_FLUX = T, CHK_GFDL_ROUGHNESS = F, CHK_FRZMLT_SST = F, USE_CORE_NYF_RUNOFF = F, USE_CORE_IAF_RUNOFF = F, CHK_A2I_FIELDS = F, CHK_I2A_FIELDS = F, CHK_I2O_FIELDS = F, CHK_O2I_FIELDS = F / MELTLIMIT = -200.000000000000 , PRECIP_FACTOR = 1.00000000000000 , CST_OCN_ALBEDO = T, OCN_ALBEDO = 0.100000000000000 , GFDL_SURFACE_FLUX = T, CHK_GFDL_ROUGHNESS = F, CHK_FRZMLT_SST = F, USE_CORE_NYF_RUNOFF = F, USE_CORE_IAF_RUNOFF = F, CHK_A2I_FIELDS = F, CHK_I2A_FIELDS = F, CHK_I2O_FIELDS = F, CHK_O2I_FIELDS = F / ICE_FWFLUX = T, LIMIT_ICEMELT = F, MELTLIMIT = -200.000000000000 , PRECIP_FACTOR = 1.00000000000000 , CST_OCN_ALBEDO = T, OCN_ALBEDO = 0.100000000000000 , GFDL_SURFACE_FLUX = T, CHK_GFDL_ROUGHNESS = F, CHK_FRZMLT_SST = F, USE_CORE_NYF_RUNOFF = F, USE_CORE_IAF_RUNOFF = F, CHK_A2I_FIELDS = F, CHK_I2A_FIELDS = F, CHK_I2O_FIELDS = F, CHK_O2I_FIELDS = F / &COUPLING_NML &COUPLING_NML DT_CPL_AI = 10800, DT_CPL_IO = 3600, POP_ICEDIAG = T, USE_OCNSLOPE = F, USE_UMASK = F, ROTATE_WINDS = F, ICE_PRESSURE_ON = T, ICE_FWFLUX = T, LIMIT_ICEMELT = F, MELTLIMIT = -200.000000000000 , PRECIP_FACTOR = 1.00000000000000 , CST_OCN_ALBEDO = T, OCN_ALBEDO = 0.100000000000000 , GFDL_SURFACE_FLUX = T, CHK_GFDL_ROUGHNESS = F, CHK_FRZMLT_SST = F, USE_CORE_NYF_RUNOFF = F, USE_CORE_IAF_RUNOFF = F, CHK_A2I_FIELDS = F, CHK_I2A_FIELDS = F, CHK_I2O_FIELDS = F, CHK_O2I_FIELDS = F / DT_CPL_AI = 10800, DT_CPL_AI = 10800, DT_CPL_IO = 3600, POP_ICEDIAG = T, USE_OCNSLOPE = F, USE_UMASK = F, ROTATE_WINDS = F, ICE_PRESSURE_ON = T, ICE_FWFLUX = T, LIMIT_ICEMELT = F, MELTLIMIT = -200.000000000000 , PRECIP_FACTOR = 1.00000000000000 , CST_OCN_ALBEDO = T, OCN_ALBEDO = 0.100000000000000 , GFDL_SURFACE_FLUX = T, CHK_GFDL_ROUGHNESS = F, CHK_FRZMLT_SST = F, USE_CORE_NYF_RUNOFF = F, USE_CORE_IAF_RUNOFF = F, DT_CPL_IO = 3600, &COUPLING_NML DT_CPL_AI = 10800, DT_CPL_IO = 3600, POP_ICEDIAG = T, USE_OCNSLOPE = F, USE_UMASK = F, ROTATE_WINDS = F, ICE_PRESSURE_ON = T, ICE_FWFLUX = T, LIMIT_ICEMELT = F, MELTLIMIT = -200.000000000000 , PRECIP_FACTOR = 1.00000000000000 , CST_OCN_ALBEDO = T, OCN_ALBEDO = 0.100000000000000 , GFDL_SURFACE_FLUX = T, CHK_GFDL_ROUGHNESS = F, CHK_FRZMLT_SST = F, USE_CORE_NYF_RUNOFF = F, USE_CORE_IAF_RUNOFF = F, CHK_A2I_FIELDS = F, CHK_I2A_FIELDS = F, CHK_I2O_FIELDS = F, CHK_O2I_FIELDS = F / POP_ICEDIAG = T, CHK_GFDL_ROUGHNESS = F, CHK_FRZMLT_SST = F, USE_CORE_NYF_RUNOFF = F, USE_CORE_IAF_RUNOFF = F, CHK_A2I_FIELDS = F, CHK_I2A_FIELDS = F, CHK_I2O_FIELDS = F, CHK_O2I_FIELDS = F / USE_OCNSLOPE = F, CHK_O2I_FIELDS = F / USE_UMASK = F, &COUPLING_NML DT_CPL_AI = 10800, DT_CPL_IO = 3600, POP_ICEDIAG = T, USE_OCNSLOPE = F, USE_UMASK = F, ROTATE_WINDS = F, ICE_PRESSURE_ON = T, ICE_FWFLUX = T, LIMIT_ICEMELT = F, MELTLIMIT = -200.000000000000 , PRECIP_FACTOR = 1.00000000000000 , CST_OCN_ALBEDO = T, OCN_ALBEDO = 0.100000000000000 , GFDL_SURFACE_FLUX = T, CHK_GFDL_ROUGHNESS = F, CHK_FRZMLT_SST = F, USE_CORE_NYF_RUNOFF = F, USE_CORE_IAF_RUNOFF = F, CHK_A2I_FIELDS = F, CHK_I2A_FIELDS = F, CHK_I2O_FIELDS = F, CHK_O2I_FIELDS = F / ROTATE_WINDS = F, CHK_A2I_FIELDS = F, CHK_I2A_FIELDS = F, CHK_I2O_FIELDS = F, CHK_O2I_FIELDS = F / ICE_PRESSURE_ON = T, ICE_FWFLUX = T, LIMIT_ICEMELT = F, MELTLIMIT = -200.000000000000 , PRECIP_FACTOR = 1.00000000000000 , CST_OCN_ALBEDO = T, OCN_ALBEDO = 0.100000000000000 , GFDL_SURFACE_FLUX = T, CHK_GFDL_ROUGHNESS = F, CHK_FRZMLT_SST = F, USE_CORE_NYF_RUNOFF = F, USE_CORE_IAF_RUNOFF = F, CHK_A2I_FIELDS = F, CHK_I2A_FIELDS = F, CHK_I2O_FIELDS = F, CHK_O2I_FIELDS = F / &COUPLING INIT_DATE = 10101, INIDATE = 10101, RUNTIME = 157680000, DT_CPL = 10800, DT_ATM = 3600, TRUNTIME0 = 0.000000000000000E+000, DATASET = jra55 , RUNTYPE = NY, CALTYPE = 0, DAYS_PER_YEAR = 365, CHK_A2I_FIELDS = F, CHK_I2A_FIELDS = F, CHK_FIELDS_PERIOD = 1 / MATM (init_calendar) idate0 = 10101 CICE: input_ice_gfdl.nml opened at unit = 35 CICE: input_ice_gfdl.nml opened at unit = 35 CICE: input_ice_gfdl.nml opened at unit = 36 CICE: input_ice_gfdl.nml opened at unit = 35 CICE: input_ice_gfdl.nml opened at unit = 35 CICE: input_ice_gfdl.nml opened at unit = 35 CICE: input_ice_gfdl.nml opened at unit = 35 CICE: input_ice_gfdl.nml opened at unit = 35 CICE: input_ice_gfdl.nml opened at unit = 35 CICE: input_ice_gfdl.nml opened at unit = 35 CICE: input_ice_gfdl.nml opened at unit = 35 CICE: input_ice_gfdl.nml opened at unit = 35 CICE: input_ice_gfdl.nml opened at unit = 35 CICE: input_ice_gfdl.nml opened at unit = 35 CICE: input_ice_gfdl.nml opened at unit = 35 CICE: input_ice_gfdl.nml opened at unit = 35 CICE: input_ice_gfdl.nml opened at unit = 35 CICE: input_ice_gfdl.nml opened at unit = 35 CICE: input_ice_gfdl.nml 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unit = 35 CICE: input_ice_gfdl.nml opened at unit = 35 CICE: input_ice_gfdl.nml opened at unit = 35 CICE: input_ice_gfdl.nml opened at unit = 35 CICE: input_ice_gfdl.nml opened at unit = 35 CICE: input_ice_gfdl.nml opened at unit = 35 CICE: input_ice_gfdl.nml opened at unit = 35 CICE: input_ice_gfdl.nml opened at unit = 35 CICE: input_ice_monin.nml opened at unit = 35 CICE: input_ice_monin.nml opened at unit = 35 CICE: input_ice_monin.nml opened at unit = 35 CICE: input_ice_monin.nml opened at unit = 35 CICE: input_ice_monin.nml opened at unit = 35 CICE: input_ice_monin.nml opened at unit = 35 CICE: input_ice_monin.nml opened at unit = 35 CICE: input_ice_monin.nml opened at unit = 35 CICE: input_ice_monin.nml opened at unit = 36 CICE: input_ice_monin.nml opened at unit = 35 CICE: input_ice_monin.nml opened at unit = 35 CICE: input_ice_monin.nml opened at unit = 35 CICE: input_ice_monin.nml opened at unit = 35 CICE: input_ice_monin.nml opened at unit = 35 CICE: input_ice_monin.nml opened at unit = 35 CICE: input_ice_monin.nml opened at unit = 35 CICE: input_ice_monin.nml opened at unit = 35 CICE: input_ice_monin.nml opened at unit = 35 CICE: input_ice_monin.nml opened at unit = 35 CICE: input_ice_monin.nml opened at unit = 35 CICE: input_ice_monin.nml opened at unit = 35 CICE: input_ice_monin.nml opened at unit = 35 CICE: input_ice_monin.nml opened at unit = 35 CICE: input_ice_monin.nml opened at unit = 35 MATM istep1: 23 idate: 10102 sec: 0 Measures of global integrated mass conservation over multiple time steps Ocean mass at timestep 3 = 1.33675573394501324E+21 kg. Ocean mass at timestep 25 = 1.33675575615703640E+21 kg. Change in ocean mass over time interval = 2.22120231567360000E+13 kg. Mass input via all contributions over time interval = 2.22120233048382227E+13 kg. Error in mass content change = -1.48102222656250000E+05 kg. Error in rate of mass content change = -1.78867418666968603E+00 kg/s. Mass input via P-E fluxes over time interval = 1.24260786247030469E+13 kg. Mass input via runoff fluxes over time interval = 9.78594468013517578E+12 kg. Mass input via ice calving fluxes over time interval = 0.00000000000000000E+00 kg. Mass input via source fluxes over time interval = 1.34277343750000000E-03 kg. Mass input via eta_t smoother over time interval = 1.34277343750000000E-03 kg. Mass input via pbot_t smoother over time interval = 0.00000000000000000E+00 kg. Measures of global integrated tracer conservation over multiple time steps Ocean heat content at timestep 5 = 1.96552398471843185E+25 J. Ocean heat content at timestep 25 = 1.96549539821386377E+25 J. Change in ocean heat content = -2.85865045680784933E+20 J. Total Heat input = -2.85874966579149406E+20 J. Error in heat content change = 9.92089835803017600E+15 J. Error in rate of heat content change = 3.31596111652309334E-04 W/m^2. Heat input by tendency terms = 6.44316800000000000E+06 J. Heat input by surface fluxes = -2.91061376462884700E+20 J. Heat input by bottom fluxes = 0.00000000000000000E+00 J. Heat input by runoff and calving = 4.94384615690320937E+14 J. Heat input by precip-evap+calving = -8.66052883228241920E+18 J. Heat input by open boundaries = 0.00000000000000000E+00 J. Heat input by frazil formation = 1.38464443314020229E+19 J. Heat input by eta_t smoother = -1.60000000000000000E+02 J. Heat input by pbot_t smoother = 0.00000000000000000E+00 J. Heat input by sources = 0.00000000000000000E+00 J. Total salt mass at timestep 5 = 4.64161483185933844E+19 kg Total salt mass at timestep 25 = 4.64161482062986691E+19 kg salt change in ocean tracer mass = -1.12294715392000000E+11 kg. salt error in mass change = 8.14137687683105469E+02 kg. salt error in rate of mass change = 2.72117384779781515E-17 kg/(m^2 sec). salt input by tendency terms = -4.63126449584960938E+01 kg. salt input by surface fluxes = -1.12294716159825195E+11 kg. salt input by bottom fluxes = 0.00000000000000000E+00 kg*yr. salt input by runoff and calving = 0.00000000000000000E+00 kg. salt input by precip-evap+calving = 0.00000000000000000E+00 kg. salt input by open boundaries = 0.00000000000000000E+00 kg*yr. salt input by eta_t smoother = 1.44958496093750000E-04 kg. salt input by pbot_t smoother = 0.00000000000000000E+00 kg. salt input by sources = 0.00000000000000000E+00 kg. Mass weighted age_global at timestep 5 = 6.07918481369541632E+17 yr*kg. Mass weighted age_global at timestep 25 = 3.78722886301037875E+18 yr*kg. age_global total tracer input = 0.00000000000000000E+00 kg*yr. age_global change in ocean tracer = 3.17931038164083712E+18 kg*yr. age_global error in tracer change = -1.40881922254510120E+16 kg*yr. age_global error in rate of tracer change = -1.48599608380548707E+04 kg/(m^2). age_global input by tendency terms = 3.25585937500000000E+00 kg*yr. age_global input by surface fluxes = 0.00000000000000000E+00 kg*yr. age_global input by bottom fluxes = 0.00000000000000000E+00 kg*yr. age_global input by runoff and calving = 0.00000000000000000E+00 kg*yr. age_global input by precip-evap+calving = 0.00000000000000000E+00 kg*yr. age_global input by open boundaries = 0.00000000000000000E+00 kg*yr. age_global input by eta_t smoother = 0.00000000000000000E+00 kg*yr. age_global input by pbot_t smoother = 0.00000000000000000E+00 kg*yr. age_global input by sources = 3.19339857386628813E+18 kg*yr. MATM istep1: 47 idate: 10103 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/ 3 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/ 3 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347692602144E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5831.9702 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347692601655E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.464853071864E+05 The minimum dzt is 4.877761758899E+00 metre at (i,j,k) = ( 49, 285, 7), (lon,lat,dpt) = ( -249.9239, 78.2035, 60.5280 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.968790364876E+04, 4.230315748901E+04, 4.877761757797E+00 m) And the number of cells in the column are kmt = 7 The grid dimensions (dst,rho_dzt) = 5.038214900672E+00, 5.048368626140E+03 yyyy/mm/dd hh:mm:ss = 1/ 1/ 3 0: 0: 0 Tracer integrals for temp The minimum T is -2.111997896077E+00 deg C at (i,j,k) = ( 241, 2, 28), (lon,lat,dpt) = ( -39.5000, -77.6297, 665.4141 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 1.374491437999E+02 m) The grid dimensions (dst,rho_dzt) = 1.380330200195E+02, 1.422584810348E+05 And the number of cells in the column are kmt = 29 The maximum T is 2.997188577546E+01 deg C at (i,j,k) = ( 49, 96, 4), (lon,lat,dpt) = ( -231.5000, -14.6898, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.075602990148E+05, 6.084705180670E+04, 1.008555899913E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.046096632332E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68310694548425666E+00 Variance temp = 2.01414216774941437E+01 |dT/dt| temp = 1.86776938634210632E+00 Total temp = 1.96547785659961616E+25 yyyy/mm/dd hh:mm:ss = 1/ 1/ 3 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/ 3 0: 0: 0 Tracer integrals for salt The maximum S is 4.059046974080E+01 psu at (i,j,k) = ( 332, 195, 1), (lon,lat,dpt) = ( 51.5000, 27.5082, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 9.904023334056E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.025205658768E+04 And the number of cells in the column are kmt = 5 The minimum S is 5.665389548457E+00 psu at (i,j,k) = ( 301, 238, 1), (lon,lat,dpt) = ( 20.5000, 61.4832, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.308624320524E+04, 5.452031705663E+04, 1.003783018184E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.038495777834E+04 And the number of cells in the column are kmt = 6 Average salt = 3.47229835447476844E+01 Variance salt = 1.47291090952421655E-01 |dT/dt| salt = 1.89825154020639209E-01 Total salt = 4.64161481965050839E+19 yyyy/mm/dd hh:mm:ss = 1/ 1/ 3 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/ 3 0: 0: 0 Tracer integrals for age_global The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.891507586777E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.024043379941E+04 And the number of cells in the column are kmt = 12 The maximum age_global is 5.361624459415E-03 yr at (i,j,k) = ( 338, 286, 4), (lon,lat,dpt) = ( 68.6757, 72.2140, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.604922695941E+04, 2.645856330123E+04, 1.002122336076E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.030182912530E+04 And the number of cells in the column are kmt = 5 Average age_global = 5.31679244646090197E-03 Variance age_global = 1.87006949487016603E-07 |dT/dt| age_global = 7.94843805730610919E-02 Total age_global = 7.10725291814152397E+18 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 1/ 3 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 2.23305408501237412E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -3.86421631815088951E+00 dbar Global max surface height on tracer cells (tau) = 1.55121332111317978E+00 m Global min surface height on tracer cells (tau) = -4.29471432776735185E+00 m Area average surface height on tracer cells (tau) = 6.41569604861206921E-05 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = 2.31822195554140625E+10 m^3 Total Mass change = -3.08970284012000000E+11 kg Mass of ocean tracer cells (tau) = 1.33675575823397683E+21 kg Mass from sources = -2.36511230468750000E-04 kg Mass from eta smoothing = -2.36511230468750000E-04 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -7.01777143495754639E+11 kg Mass of river runoff liquid water input = 3.27295436194560289E+08 kg Mass of sea ice melt input = 3.92479563885444092E+11 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = 1.62116223096847534E+02 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96547785659961616E+25 J Total heat change of full system for (taup1-taum1) = 3.36177168311485481E+19 J Total heat input to ocean referenced to 0degC = 3.36174446750478541E+19 J Heat input via surface heat fluxes = 3.35452674067340616E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -3.07690184301665408E+17 J Heat input via river runoff = 2.32769297677784687E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 3.79844175685690496E+17 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = 1.29512153125000000E+06 J Heat input via eta_t smooth = 1.20000000000000000E+01 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 3.36177168311485481E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 2.72156099398894469E+14 J Mismatch converted to a surface flux = 2.09220548837896008E-04 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161481965050839E+19 kg Total tracer change in system for (taup1-taum1) = 1.56991331258007812E+09 kg Total tracer input to ocean = 1.56991330506301737E+09 kg Tracer input via surface fluxes = 1.56991330506301880E+09 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = 2.55859518051147461E+00 kg Tracer input via eta_t smoother = -1.43051147460937500E-06 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 1.57755408067240524E+09 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = 4.98259842813110332E+00 kg Mismatch converted to a surface flux = 3.83038256381132621E-18 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 5.31679244646090197E-03 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066637410675648E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13757981971757260E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13757981971757246E-04 yr Age input via sources in th_tendency, or errors = -2.37610312311681973E-21 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.12874853158415826E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -8.83128813341439593E-07 yr Mismatch converted to a surface flux = -2.14246771720354951E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 71 idate: 10104 sec: 0 MATM istep1: 95 idate: 10105 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/ 5 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/ 5 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347778038127E+02 metre at (i,j,k) = ( 53, 185, 50), (lon,lat,dpt) = ( -227.5000, 18.5866, 5832.1191 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.053953113392E+05, 8.372307267313E+04, 3.347778037638E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.464949453129E+05 The minimum dzt is 4.819719788912E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 40.1266 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.819719787827E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.987501611000E+03 yyyy/mm/dd hh:mm:ss = 1/ 1/ 5 0: 0: 0 Tracer integrals for temp The minimum T is -2.109166116935E+00 deg C at (i,j,k) = ( 241, 3, 29), (lon,lat,dpt) = ( -39.5000, -77.3817, 812.7816 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.429106759255E+04, 2.765537186494E+04, 5.024345832418E+01 m) The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.200351669727E+04 And the number of cells in the column are kmt = 29 The maximum T is 3.002967286718E+01 deg C at (i,j,k) = ( 49, 96, 1), (lon,lat,dpt) = ( -231.5000, -14.6898, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.075602990148E+05, 6.084705180670E+04, 1.013227696886E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.048252009866E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68308584763936553E+00 Variance temp = 2.01372267782728258E+01 |dT/dt| temp = 2.07395433239251492E+00 Total temp = 1.96546654564716904E+25 yyyy/mm/dd hh:mm:ss = 1/ 1/ 5 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/ 5 0: 0: 0 Tracer integrals for salt The maximum S is 4.059185807077E+01 psu at (i,j,k) = ( 332, 195, 5), (lon,lat,dpt) = ( 51.5000, 27.5082, 45.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 9.919836040098E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.026590221299E+04 And the number of cells in the column are kmt = 5 The minimum S is 5.713438147016E+00 psu at (i,j,k) = ( 301, 238, 1), (lon,lat,dpt) = ( 20.5000, 61.4832, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.308624320524E+04, 5.452031705663E+04, 9.980933664879E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.033283395318E+04 And the number of cells in the column are kmt = 6 Average salt = 3.47229845997329178E+01 Variance salt = 1.47076494428119986E-01 |dT/dt| salt = 2.14955056864684746E-01 Total salt = 4.64161483750263521E+19 yyyy/mm/dd hh:mm:ss = 1/ 1/ 5 0: 0: 0 The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.870381343787E+00 m) yyyy/mm/dd hh:mm:ss = 1/ 1/ 5 0: 0: 0 Tracer integrals for age_global The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021608453517E+04 And the number of cells in the column are kmt = 12 The maximum age_global is 1.083732603499E-02 yr at (i,j,k) = ( 341, 292, 3), (lon,lat,dpt) = ( 74.0335, 71.8968, 25.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.645608625640E+04, 2.424195933219E+04, 9.905267907299E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.024889420096E+04 And the number of cells in the column are kmt = 5 Average age_global = 1.07220100109385024E-02 Variance age_global = 1.02098926398785277E-06 |dT/dt| age_global = 7.98004751080025609E-02 Total age_global = 1.43327082416200909E+19 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 1/ 5 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.71059525590725259E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -3.73525523683317040E+00 dbar Global max surface height on tracer cells (tau) = 1.16324012683442279E+00 m Global min surface height on tracer cells (tau) = -4.16205653607934245E+00 m Area average surface height on tracer cells (tau) = -3.06956124080400068E-05 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -1.10914298439218750E+10 m^3 Total Mass change = -1.01328163057171875E+12 kg Mass of ocean tracer cells (tau) = 1.33675572276074958E+21 kg Mass from sources = -6.10351562500000000E-05 kg Mass from eta smoothing = -6.10351562500000000E-05 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -2.28903228453080273E+12 kg Mass of river runoff liquid water input = 3.24996008984009981E+08 kg Mass of sea ice melt input = 1.27542565743735620E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = 5.12743590116500854E+02 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96546654564716904E+25 J Total heat change of full system for (taup1-taum1) = 3.93390182202879672E+19 J Total heat input to ocean referenced to 0degC = 3.93388538904131092E+19 J Heat input via surface heat fluxes = 3.95165897439632835E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -4.07111977348427648E+17 J Heat input via river runoff = 2.33999053166856172E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 2.29352723892937952E+17 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = -9.74753617187500000E+05 J Heat input via eta_t smooth = -4.40000000000000000E+01 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 3.93390182202879672E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 1.64329875832737625E+14 J Mismatch converted to a surface flux = 1.26328922585698742E-04 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161483750263521E+19 kg Total tracer change in system for (taup1-taum1) = 5.10169619227148437E+09 kg Total tracer input to ocean = 5.10169616529496765E+09 kg Tracer input via surface fluxes = 5.10169616529496765E+09 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = -2.25097680091857910E+00 kg Tracer input via eta_t smoother = 2.38418579101562500E-07 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 5.12652614763926983E+09 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = 2.93697437355353834E+01 kg Mismatch converted to a surface flux = 2.25780495720980018E-17 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 1.07220100109385024E-02 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066678367712512E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758015689601085E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758015689601112E-04 yr Age input via sources in th_tendency, or errors = 2.17301120091914180E-21 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.12585594728382204E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -1.17242096121888867E-06 yr Mismatch converted to a surface flux = -2.84428955599376452E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 119 idate: 10106 sec: 0 MATM istep1: 143 idate: 10107 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/ 7 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/ 7 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347833203796E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5832.2152 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347833203308E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.465007134471E+05 The minimum dzt is 4.805963199472E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 40.0121 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.805963198390E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.975946702360E+03 The minimum T is -2.108358558349E+00 deg C at (i,j,k) = ( 241, 2, 29), (lon,lat,dpt) = ( -39.5000, -77.6297, 812.7816 m) yyyy/mm/dd hh:mm:ss = 1/ 1/ 7 0: 0: 0 Tracer integrals for temp The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 5.024693162640E+01 m) The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.200557763729E+04 And the number of cells in the column are kmt = 29 The maximum T is 3.010715478825E+01 deg C at (i,j,k) = ( 49, 96, 4), (lon,lat,dpt) = ( -231.5000, -14.6898, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.075602990148E+05, 6.084705180670E+04, 1.012948622605E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.048395748895E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68312704229982657E+00 Variance temp = 2.01347239658374306E+01 |dT/dt| temp = 2.16778439261873546E+00 Total temp = 1.96548844499058915E+25 yyyy/mm/dd hh:mm:ss = 1/ 1/ 7 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/ 7 0: 0: 0 Tracer integrals for salt The maximum S is 4.059607422489E+01 psu at (i,j,k) = ( 332, 195, 4), (lon,lat,dpt) = ( 51.5000, 27.5082, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 9.912172384423E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.025856773700E+04 And the number of cells in the column are kmt = 5 The minimum S is 5.743234733834E+00 psu at (i,j,k) = ( 300, 238, 1), (lon,lat,dpt) = ( 19.5000, 61.4832, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.308624320524E+04, 5.452031705663E+04, 9.996384013146E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.034689923854E+04 And the number of cells in the column are kmt = 9 Average salt = 3.47229863007956041E+01 Variance salt = 1.46924116167156171E-01 |dT/dt| salt = 2.41546352735651976E-01 Total salt = 4.64161486640305766E+19 yyyy/mm/dd hh:mm:ss = 1/ 1/ 7 0: 0: 0 The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.873608322250E+00 m) yyyy/mm/dd hh:mm:ss = 1/ 1/ 7 0: 0: 0 Tracer integrals for age_global The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021940779297E+04 And the number of cells in the column are kmt = 12 The maximum age_global is 1.631302761056E-02 yr at (i,j,k) = ( 341, 292, 4), (lon,lat,dpt) = ( 74.0335, 71.8968, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.645608625640E+04, 2.424195933219E+04, 9.866957233520E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.023005641136E+04 And the number of cells in the column are kmt = 5 Average age_global = 1.61155917861905557E-02 Variance age_global = 2.69217680758701127E-06 |dT/dt| age_global = 8.02576413591076232E-02 Total age_global = 2.15426086246363996E+19 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 1/ 7 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.66337095846198513E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -3.54963985413443295E+00 dbar Global max surface height on tracer cells (tau) = 1.08975725051285877E+00 m Global min surface height on tracer cells (tau) = -3.94925304252536113E+00 m Area average surface height on tracer cells (tau) = -1.83547289915117598E-04 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -6.63222437810781326E+10 m^3 Total Mass change = -1.33457508325085938E+12 kg Mass of ocean tracer cells (tau) = 1.33675566559685719E+21 kg Mass from sources = 1.18255615234375000E-04 kg Mass from eta smoothing = 1.18255615234375000E-04 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -3.01353579125532959E+12 kg Mass of river runoff liquid water input = 3.22552310644589305E+08 kg Mass of sea ice melt input = 1.67863815552525928E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = 1.68566229939460754E+02 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96548844499058915E+25 J Total heat change of full system for (taup1-taum1) = 4.98293099015212810E+19 J Total heat input to ocean referenced to 0degC = 4.98291269691099955E+19 J Heat input via surface heat fluxes = 4.99336626676821524E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -3.59875262984138112E+17 J Heat input via river runoff = 2.35641830804746992E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 2.55316000228900096E+17 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = 2.03553230078125000E+06 J Heat input via eta_t smooth = 2.50000000000000000E+01 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 4.98293099015212810E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 1.82932409249971687E+14 J Mismatch converted to a surface flux = 1.40629657568031518E-04 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161486640305766E+19 kg Total tracer change in system for (taup1-taum1) = 6.71454482703027344E+09 kg Total tracer input to ocean = 6.71454481636641884E+09 kg Tracer input via surface fluxes = 6.71454481636640930E+09 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = 7.81240463256835938E-01 kg Tracer input via eta_t smoother = 9.53674316406250000E-06 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 6.74722451670342922E+09 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = 9.93071281874084377E+00 kg Mismatch converted to a surface flux = 7.63425545441561601E-18 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 1.61155917861905557E-02 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066714944416704E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758047943891117E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758047943891144E-04 yr Age input via sources in th_tendency, or errors = 2.82940754516069691E-21 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.12385345940571872E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -1.37270200331924605E-06 yr Mismatch converted to a surface flux = -3.33017073276610655E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 167 idate: 10108 sec: 0 MATM istep1: 191 idate: 10109 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/ 9 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/ 9 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347835386110E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5832.2190 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347835385621E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.465009766928E+05 The minimum dzt is 4.795340640788E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 39.9237 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.795340639709E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.962222407100E+03 yyyy/mm/dd hh:mm:ss = 1/ 1/ 9 0: 0: 0 Tracer integrals for temp The minimum T is -2.107461115260E+00 deg C at (i,j,k) = ( 241, 2, 29), (lon,lat,dpt) = ( -39.5000, -77.6297, 812.7816 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 5.024647450886E+01 m) The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.200526915854E+04 And the number of cells in the column are kmt = 29 The maximum T is 3.016291244924E+01 deg C at (i,j,k) = ( 49, 96, 1), (lon,lat,dpt) = ( -231.5000, -14.6898, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.075602990148E+05, 6.084705180670E+04, 1.014790291587E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.050380871335E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68321985260195950E+00 Variance temp = 2.01345122036487112E+01 |dT/dt| temp = 2.07253702791195460E+00 Total temp = 1.96553786796853318E+25 yyyy/mm/dd hh:mm:ss = 1/ 1/ 9 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/ 9 0: 0: 0 Tracer integrals for salt The maximum S is 4.060071701860E+01 psu at (i,j,k) = ( 332, 195, 2), (lon,lat,dpt) = ( 51.5000, 27.5082, 15.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 9.904950558940E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.025153347894E+04 And the number of cells in the column are kmt = 5 The minimum S is 5.764363211431E+00 psu at (i,j,k) = ( 300, 238, 1), (lon,lat,dpt) = ( 19.5000, 61.4832, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.308624320524E+04, 5.452031705663E+04, 9.995741310347E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.034516910778E+04 And the number of cells in the column are kmt = 9 Average salt = 3.47229884237426347E+01 Variance salt = 1.46799850623665407E-01 |dT/dt| salt = 2.37061063297844155E-01 Total salt = 4.64161490239759483E+19 yyyy/mm/dd hh:mm:ss = 1/ 1/ 9 0: 0: 0 The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.870709532493E+00 m) yyyy/mm/dd hh:mm:ss = 1/ 1/ 9 0: 0: 0 Tracer integrals for age_global The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021612434192E+04 And the number of cells in the column are kmt = 12 The maximum age_global is 2.178872918613E-02 yr at (i,j,k) = ( 338, 283, 4), (lon,lat,dpt) = ( 66.7661, 71.8192, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.655653313420E+04, 2.615321824693E+04, 9.861293833095E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.022944048158E+04 And the number of cells in the column are kmt = 6 Average age_global = 2.15034032906372685E-02 Variance age_global = 5.26629590864727617E-06 |dT/dt| age_global = 8.08098023211612504E-02 Total age_global = 2.87447946438388040E+19 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 1/ 9 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.61927314523085952E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -3.44191853050626850E+00 dbar Global max surface height on tracer cells (tau) = 1.05565658511298910E+00 m Global min surface height on tracer cells (tau) = -3.92674891003576665E+00 m Area average surface height on tracer cells (tau) = -3.74364666707200321E-04 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -1.35271431683132813E+11 m^3 Total Mass change = -1.61741407323795313E+12 kg Mass of ocean tracer cells (tau) = 1.33675559423444779E+21 kg Mass from sources = -1.90734863281250000E-05 kg Mass from eta smoothing = -1.90734863281250000E-05 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -3.65882325002721289E+12 kg Mass of river runoff liquid water input = 3.22869786681453466E+08 kg Mass of sea ice melt input = 2.04108630690412671E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = 9.84513781070709229E+01 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96553786796853318E+25 J Total heat change of full system for (taup1-taum1) = 4.55735042329028854E+19 J Total heat input to ocean referenced to 0degC = 4.55733627495601603E+19 J Heat input via surface heat fluxes = 4.56471713292401705E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -2.71298854960967616E+17 J Heat input via river runoff = 2.41016288597668203E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 1.97466173652087488E+17 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = 1.98973117968750000E+06 J Heat input via eta_t smooth = -2.60000000000000000E+01 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 4.55735042329028854E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 1.41483340735388812E+14 J Mismatch converted to a surface flux = 1.08765602775233406E-04 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161490239759483E+19 kg Total tracer change in system for (taup1-taum1) = 8.16433666776660156E+09 kg Total tracer input to ocean = 8.16433666065335083E+09 kg Tracer input via surface fluxes = 8.16433666065335083E+09 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = 4.89355421066284180E+00 kg Tracer input via eta_t smoother = 4.76837158203125000E-07 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 8.20407249432862091E+09 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = 2.23049978473043442E+00 kg Mismatch converted to a surface flux = 1.71470119602252784E-18 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 2.15034032906372685E-02 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066715435533536E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758054408304269E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758054408304241E-04 yr Age input via sources in th_tendency, or errors = 5.44768737286014858E-21 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.12319829813449420E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -1.43822459485484673E-06 yr Mismatch converted to a surface flux = -3.48912833327898283E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 215 idate: 10110 sec: 0 MATM istep1: 239 idate: 10111 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/11 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/11 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347841818146E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5832.2302 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347841817657E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.465016464319E+05 The minimum dzt is 4.786784396547E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 39.8524 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.786784395470E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.955915953057E+03 yyyy/mm/dd hh:mm:ss = 1/ 1/11 0: 0: 0 Tracer integrals for temp The minimum T is -2.106368884898E+00 deg C at (i,j,k) = ( 241, 2, 29), (lon,lat,dpt) = ( -39.5000, -77.6297, 812.7816 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 5.024441698722E+01 m) The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.200288571900E+04 And the number of cells in the column are kmt = 29 The maximum T is 3.023780712732E+01 deg C at (i,j,k) = ( 49, 96, 4), (lon,lat,dpt) = ( -231.5000, -14.6898, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.075602990148E+05, 6.084705180670E+04, 1.014098326693E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.049663123600E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68329984187380832E+00 Variance temp = 2.01334468678547793E+01 |dT/dt| temp = 2.12811626340779103E+00 Total temp = 1.96558042949927538E+25 yyyy/mm/dd hh:mm:ss = 1/ 1/11 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/11 0: 0: 0 Tracer integrals for salt The maximum S is 4.060446587238E+01 psu at (i,j,k) = ( 332, 195, 2), (lon,lat,dpt) = ( 51.5000, 27.5082, 15.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 9.899274298629E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.024525405579E+04 And the number of cells in the column are kmt = 5 The minimum S is 5.862677335517E+00 psu at (i,j,k) = ( 300, 238, 1), (lon,lat,dpt) = ( 19.5000, 61.4832, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.308624320524E+04, 5.452031705663E+04, 1.000323428324E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.035400744227E+04 And the number of cells in the column are kmt = 9 Average salt = 3.47229909410067563E+01 Variance salt = 1.46708360422280748E-01 |dT/dt| salt = 2.31537398974704184E-01 Total salt = 4.64161494495370281E+19 yyyy/mm/dd hh:mm:ss = 1/ 1/11 0: 0: 0 The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) yyyy/mm/dd hh:mm:ss = 1/ 1/11 0: 0: 0 Tracer integrals for age_global The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.868199731090E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021359264760E+04 And the number of cells in the column are kmt = 12 The maximum age_global is 2.726443076171E-02 yr at (i,j,k) = ( 338, 283, 4), (lon,lat,dpt) = ( 66.7661, 71.8192, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.655653313420E+04, 2.615321824693E+04, 9.841303164457E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021719478119E+04 And the number of cells in the column are kmt = 6 Average age_global = 2.68868933062734947E-02 Variance age_global = 8.79942923981945086E-06 |dT/dt| age_global = 8.16592825091650848E-02 Total age_global = 3.59412027626892902E+19 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 1/11 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.63024374357722701E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -3.33386353522725409E+00 dbar Global max surface height on tracer cells (tau) = 1.04700218597093220E+00 m Global min surface height on tracer cells (tau) = -3.85356921940195063E+00 m Area average surface height on tracer cells (tau) = -6.00720055017186887E-04 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -2.17061782560000000E+11 m^3 Total Mass change = -1.86488856464420996E+12 kg Mass of ocean tracer cells (tau) = 1.33675550958143485E+21 kg Mass from sources = -2.09808349609375000E-04 kg Mass from eta smoothing = -2.09808349609375000E-04 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -4.20998972447305957E+12 kg Mass of river runoff liquid water input = 3.30570709915634215E+08 kg Mass of sea ice melt input = 2.34477058908902734E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = 2.99068412184715271E+01 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96558042949927538E+25 J Total heat change of full system for (taup1-taum1) = 5.20368494309430477E+19 J Total heat input to ocean referenced to 0degC = 5.20367359540761149E+19 J Heat input via surface heat fluxes = 5.21982000567478436E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -3.19867519803363584E+17 J Heat input via river runoff = 2.54670682781666719E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 1.58377950063365984E+17 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = 8.81517328125000000E+05 J Heat input via eta_t smooth = -4.00000000000000000E+00 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 5.20368494309430477E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 1.13476866051218672E+14 J Mismatch converted to a surface flux = 8.72355690285029879E-05 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161494495370281E+19 kg Total tracer change in system for (taup1-taum1) = 9.37907334781582642E+09 kg Total tracer input to ocean = 9.37907334642012215E+09 kg Tracer input via surface fluxes = 9.37907334642012024E+09 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = -1.92807269096374512E+00 kg Tracer input via eta_t smoother = 2.62260437011718750E-06 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 9.42472129779964638E+09 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = 3.33995378283905975E+00 kg Mismatch converted to a surface flux = 2.56759618866595755E-18 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 2.68868933062734912E-02 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066717202000032E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758062954804134E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758062954804121E-04 yr Age input via sources in th_tendency, or errors = -2.17173309189056745E-21 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.12271682620749324E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -1.48638033405482261E-06 yr Mismatch converted to a surface flux = -3.60595400477265319E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 263 idate: 10112 sec: 0 MATM istep1: 287 idate: 10113 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/13 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/13 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347843022539E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5832.2323 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347843022050E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.465017845382E+05 The minimum dzt is 4.774598890791E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 39.7510 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.774598889717E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.941192508193E+03 yyyy/mm/dd hh:mm:ss = 1/ 1/13 0: 0: 0 Tracer integrals for temp The minimum T is -2.105075618007E+00 deg C at (i,j,k) = ( 241, 2, 29), (lon,lat,dpt) = ( -39.5000, -77.6297, 812.7816 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 5.024742447288E+01 m) The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.200605863298E+04 And the number of cells in the column are kmt = 29 The maximum T is 3.027485251910E+01 deg C at (i,j,k) = ( 49, 96, 4), (lon,lat,dpt) = ( -231.5000, -14.6898, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.075602990148E+05, 6.084705180670E+04, 1.014113585681E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.049672994832E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68340854674146678E+00 Variance temp = 2.01329159490064100E+01 |dT/dt| temp = 2.01300907801001738E+00 Total temp = 1.96563830240520193E+25 yyyy/mm/dd hh:mm:ss = 1/ 1/13 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/13 0: 0: 0 Tracer integrals for salt The maximum S is 4.060640743122E+01 psu at (i,j,k) = ( 332, 195, 4), (lon,lat,dpt) = ( 51.5000, 27.5082, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 9.908394917352E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.025507881121E+04 And the number of cells in the column are kmt = 5 The minimum S is 5.911973705048E+00 psu at (i,j,k) = ( 298, 238, 1), (lon,lat,dpt) = ( 17.5000, 61.4832, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.308624320524E+04, 5.452031705663E+04, 9.990344099351E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.034048356891E+04 And the number of cells in the column are kmt = 5 Average salt = 3.47229937134162654E+01 Variance salt = 1.46637712767414996E-01 |dT/dt| salt = 2.26441006908613796E-01 Total salt = 4.64161499186676941E+19 yyyy/mm/dd hh:mm:ss = 1/ 1/13 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/13 0: 0: 0 Tracer integrals for age_global The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.870902196011E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021644811770E+04 And the number of cells in the column are kmt = 12 The maximum age_global is 3.274013233728E-02 yr at (i,j,k) = ( 338, 283, 4), (lon,lat,dpt) = ( 66.7661, 71.8192, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.655653313420E+04, 2.615321824693E+04, 9.852914085622E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.022407093194E+04 And the number of cells in the column are kmt = 6 Average age_global = 3.22658172474254781E-02 Variance age_global = 1.33438429973226341E-05 |dT/dt| age_global = 8.21615697590193927E-02 Total age_global = 4.31315059688004813E+19 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 1/13 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.63674802124612051E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -3.16290906869685307E+00 dbar Global max surface height on tracer cells (tau) = 9.86891383241058184E-01 m Global min surface height on tracer cells (tau) = -3.79764535505290635E+00 m Area average surface height on tracer cells (tau) = -8.49984847964507339E-04 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -3.07130126099898438E+11 m^3 Total Mass change = -1.97755389071765625E+12 kg Mass of ocean tracer cells (tau) = 1.33675541636069930E+21 kg Mass from sources = -2.28881835937500000E-04 kg Mass from eta smoothing = -2.28881835937500000E-04 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -4.46959639244172363E+12 kg Mass of river runoff liquid water input = 3.53170344592217207E+08 kg Mass of sea ice melt input = 2.49168933151473633E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = -1.35260933637619019E+02 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96563830240520193E+25 J Total heat change of full system for (taup1-taum1) = 4.37637750878913987E+19 J Total heat input to ocean referenced to 0degC = 4.37636654790701056E+19 J Heat input via surface heat fluxes = 4.40190448494727660E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -4.08386661375536640E+17 J Heat input via river runoff = 2.79244407727448398E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 1.52979366532098688E+17 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = 1.30190716015625000E+06 J Heat input via eta_t smooth = -2.80000000000000000E+01 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 4.37637750878913987E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 1.09608819991148844E+14 J Mismatch converted to a surface flux = 8.42620008394912511E-05 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161499186676941E+19 kg Total tracer change in system for (taup1-taum1) = 9.96674789032861328E+09 kg Total tracer input to ocean = 9.96674787522862434E+09 kg Tracer input via surface fluxes = 9.96674787522862244E+09 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = 5.10009503364562988E+00 kg Tracer input via eta_t smoother = 2.62260437011718750E-06 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 1.00152560523108425E+10 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = 1.00485633873617637E+01 kg Mismatch converted to a surface flux = 7.72485331609200666E-18 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 3.22658172474254781E-02 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066708290872832E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758064231252862E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758064231252862E-04 yr Age input via sources in th_tendency, or errors = -4.20699119764841458E-21 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.12163921141364442E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -1.59414308988842156E-06 yr Mismatch converted to a surface flux = -3.86738611071517634E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 311 idate: 10114 sec: 0 MATM istep1: 335 idate: 10115 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/15 0: 0: 0 The minimum T is -2.103586780091E+00 deg C at (i,j,k) = ( 241, 2, 29), (lon,lat,dpt) = ( -39.5000, -77.6297, 812.7816 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 5.024869933667E+01 m) The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.200752932646E+04 And the number of cells in the column are kmt = 29 yyyy/mm/dd hh:mm:ss = 1/ 1/15 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/15 0: 0: 0 Tracer integrals for temp Average temp = 3.68345883484436820E+00 Variance temp = 2.01312138066218509E+01 |dT/dt| temp = 1.79474912120075802E+00 Total temp = 1.96566499149442654E+25 yyyy/mm/dd hh:mm:ss = 1/ 1/15 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/15 0: 0: 0 Tracer integrals for salt The minimum S is 5.938620091386E+00 psu at (i,j,k) = ( 298, 237, 1), (lon,lat,dpt) = ( 17.5000, 60.9889, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.392724994408E+04, 5.550566181049E+04, 9.975057672132E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.032546250460E+04 And the number of cells in the column are kmt = 5 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347843663843E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5832.2334 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347843663354E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.465018042161E+05 The maximum T is 3.033832772002E+01 deg C at (i,j,k) = ( 49, 96, 4), (lon,lat,dpt) = ( -231.5000, -14.6898, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.075602990148E+05, 6.084705180670E+04, 1.013358027687E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.048728836436E+04 And the number of cells in the column are kmt = 5 The minimum dzt is 4.786743070810E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 39.8521 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.786743069733E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.955197196586E+03 The maximum S is 4.060492134148E+01 psu at (i,j,k) = ( 332, 195, 2), (lon,lat,dpt) = ( 51.5000, 27.5082, 15.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 9.937542449089E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.028515280062E+04 And the number of cells in the column are kmt = 5 Average salt = 3.47229966875422846E+01 Variance salt = 1.46567610951024108E-01 |dT/dt| salt = 2.10934695127896393E-01 Total salt = 4.64161504235477238E+19 yyyy/mm/dd hh:mm:ss = 1/ 1/15 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/15 0: 0: 0 Tracer integrals for age_global The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.868352521773E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021389679246E+04 And the number of cells in the column are kmt = 12 The maximum age_global is 3.821583391285E-02 yr at (i,j,k) = ( 338, 283, 4), (lon,lat,dpt) = ( 66.7661, 71.8192, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.655653313420E+04, 2.615321824693E+04, 9.841764935748E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021833199747E+04 And the number of cells in the column are kmt = 6 Average age_global = 3.76392486804119214E-02 Variance age_global = 1.90361899504330398E-05 |dT/dt| age_global = 8.26279623168841987E-02 Total age_global = 5.03144657789897277E+19 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 1/15 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.64600459678992639E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -3.02718648001560942E+00 dbar Global max surface height on tracer cells (tau) = 1.11591779360545074E+00 m Global min surface height on tracer cells (tau) = -3.76455978426121840E+00 m Area average surface height on tracer cells (tau) = -1.11726129295425507E-03 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -4.03706727964996094E+11 m^3 Total Mass change = -2.15607283924642871E+12 kg Mass of ocean tracer cells (tau) = 1.33675531640391624E+21 kg Mass from sources = 3.81469726562500000E-06 kg Mass from eta smoothing = 3.81469726562500000E-06 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -4.86549114130868555E+12 kg Mass of river runoff liquid water input = 3.70425551509291112E+08 kg Mass of sea ice melt input = 2.70904787635966992E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = 1.51077619135379791E+02 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96566499149442654E+25 J Total heat change of full system for (taup1-taum1) = 4.76516981332096696E+19 J Total heat input to ocean referenced to 0degC = 4.76515988489339945E+19 J Heat input via surface heat fluxes = 4.78970722329377014E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -3.84072791746905024E+17 J Heat input via river runoff = 2.98492509940547500E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 1.38569558492199456E+17 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = 2.15968525000000000E+06 J Heat input via eta_t smooth = -1.20000000000000000E+01 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 4.76516981332096696E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 9.92842735154507500E+13 J Mismatch converted to a surface flux = 7.63249849691179419E-05 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161504235477238E+19 kg Total tracer change in system for (taup1-taum1) = 1.08361817200145264E+10 kg Total tracer input to ocean = 1.08361816982740173E+10 kg Tracer input via surface fluxes = 1.08361816982740173E+10 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = 2.88339138031005859E+00 kg Tracer input via eta_t smoother = 9.53674316406250000E-07 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 1.08889214164458370E+10 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = 1.89488952445096963E+01 kg Mismatch converted to a surface flux = 1.45670013337361208E-17 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 3.76392486804119214E-02 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066702464607680E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758068394268213E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758068394268199E-04 yr Age input via sources in th_tendency, or errors = -1.22877994760337644E-20 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.12037842708346394E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -1.72022568592181808E-06 yr Mismatch converted to a surface flux = -4.17326209123120336E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 359 idate: 10116 sec: 0 MATM istep1: 383 idate: 10117 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/17 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/17 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347848421619E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5832.2417 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347848421130E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.465023284613E+05 The minimum dzt is 4.775037150315E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 39.7546 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.775037149241E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.942798153307E+03 The minimum T is -2.101913024981E+00 deg C at (i,j,k) = ( 241, 2, 29), (lon,lat,dpt) = ( -39.5000, -77.6297, 812.7816 m) yyyy/mm/dd hh:mm:ss = 1/ 1/17 0: 0: 0 Tracer integrals for temp The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 5.025030975651E+01 m) The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.200896422864E+04 And the number of cells in the column are kmt = 29 The maximum T is 3.039877316974E+01 deg C at (i,j,k) = ( 49, 96, 2), (lon,lat,dpt) = ( -231.5000, -14.6898, 15.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.075602990148E+05, 6.084705180670E+04, 1.013107263303E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.048515716411E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68349448624692632E+00 Variance temp = 2.01295567155129866E+01 |dT/dt| temp = 1.80038302090717472E+00 Total temp = 1.96568386059662784E+25 yyyy/mm/dd hh:mm:ss = 1/ 1/17 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/17 0: 0: 0 Tracer integrals for salt The maximum S is 4.060180178893E+01 psu at (i,j,k) = ( 332, 195, 3), (lon,lat,dpt) = ( 51.5000, 27.5082, 25.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 9.979968323532E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.032786587592E+04 And the number of cells in the column are kmt = 5 The minimum S is 5.978428075671E+00 psu at (i,j,k) = ( 298, 237, 1), (lon,lat,dpt) = ( 17.5000, 60.9889, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.392724994408E+04, 5.550566181049E+04, 9.921508949191E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.026912308282E+04 And the number of cells in the column are kmt = 5 Average salt = 3.47229998510758762E+01 Variance salt = 1.46512856170375017E-01 |dT/dt| salt = 2.11113198334427543E-01 Total salt = 4.64161509653361050E+19 yyyy/mm/dd hh:mm:ss = 1/ 1/17 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/17 0: 0: 0 Tracer integrals for age_global The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.867865449087E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021324245092E+04 And the number of cells in the column are kmt = 12 The maximum age_global is 4.369153548843E-02 yr at (i,j,k) = ( 338, 281, 4), (lon,lat,dpt) = ( 65.6026, 71.5268, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.693914597147E+04, 2.592186576923E+04, 9.850885527939E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.019614322844E+04 And the number of cells in the column are kmt = 9 Average age_global = 4.30061183251028295E-02 Variance age_global = 2.60274907507322337E-05 |dT/dt| age_global = 8.34996822914871040E-02 Total age_global = 5.74886527423473746E+19 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 1/17 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.64291426378153282E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -2.92888828164776793E+00 dbar Global max surface height on tracer cells (tau) = 9.99412530296487911E-01 m Global min surface height on tracer cells (tau) = -3.75980058410089768E+00 m Area average surface height on tracer cells (tau) = -1.40119304987917741E-03 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -5.06301493644582031E+11 m^3 Total Mass change = -2.26893121055173730E+12 kg Mass of ocean tracer cells (tau) = 1.33675521021833380E+21 kg Mass from sources = -1.14440917968750000E-05 kg Mass from eta smoothing = -1.14440917968750000E-05 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -5.13245814778877148E+12 kg Mass of river runoff liquid water input = 3.74330810185410500E+08 kg Mass of sea ice melt input = 2.86315260632964209E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = 9.72071790695190430E+01 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96568386059662784E+25 J Total heat change of full system for (taup1-taum1) = 4.35562580833917010E+19 J Total heat input to ocean referenced to 0degC = 4.35561670563173089E+19 J Heat input via surface heat fluxes = 4.37546203865699779E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -3.25528579014600640E+17 J Heat input via river runoff = 3.01364750840767266E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 1.27045112286846880E+17 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = -2.08727265625000000E+04 J Heat input via eta_t smooth = 2.80000000000000000E+01 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 4.35562580833917010E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 9.10270744129367187E+13 J Mismatch converted to a surface flux = 6.99772465502200027E-05 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161509653361050E+19 kg Total tracer change in system for (taup1-taum1) = 1.14526004077035522E+10 kg Total tracer input to ocean = 1.14526004031078815E+10 kg Tracer input via surface fluxes = 1.14526004031078796E+10 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = 4.65685892105102539E+00 kg Tracer input via eta_t smoother = 1.43051147460937500E-06 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 1.15083402138878441E+10 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = -6.14860240492820717E-02 kg Mismatch converted to a surface flux = -4.72675046631827351E-20 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 4.30061183251028295E-02 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066698232770464E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758074274528155E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758074274528155E-04 yr Age input via sources in th_tendency, or errors = 6.93581316898144788E-21 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.11958099583760998E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -1.79997469076716876E-06 yr Mismatch converted to a surface flux = -4.36673292558638930E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 407 idate: 10118 sec: 0 MATM istep1: 431 idate: 10119 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/19 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/19 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347846603815E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5832.2385 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347846603327E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.465020897317E+05 The minimum dzt is 4.770248186895E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 39.7148 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.770248185821E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.937261690756E+03 The minimum T is -2.100065406520E+00 deg C at (i,j,k) = ( 241, 2, 29), (lon,lat,dpt) = ( -39.5000, -77.6297, 812.7816 m) yyyy/mm/dd hh:mm:ss = 1/ 1/19 0: 0: 0 Tracer integrals for temp The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 5.025101676065E+01 m) The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.200990271708E+04 And the number of cells in the column are kmt = 29 The maximum T is 3.040524552596E+01 deg C at (i,j,k) = ( 49, 96, 4), (lon,lat,dpt) = ( -231.5000, -14.6898, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.075602990148E+05, 6.084705180670E+04, 1.013074654774E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.048562056695E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68353561440124944E+00 Variance temp = 2.01284667198214109E+01 |dT/dt| temp = 1.70885293200542732E+00 Total temp = 1.96570564700114228E+25 yyyy/mm/dd hh:mm:ss = 1/ 1/19 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/19 0: 0: 0 Tracer integrals for salt The maximum S is 4.059889765646E+01 psu at (i,j,k) = ( 332, 195, 1), (lon,lat,dpt) = ( 51.5000, 27.5082, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 1.000460717801E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.035456377817E+04 And the number of cells in the column are kmt = 5 The minimum S is 6.030356474550E+00 psu at (i,j,k) = ( 298, 237, 1), (lon,lat,dpt) = ( 17.5000, 60.9889, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.392724994408E+04, 5.550566181049E+04, 9.946754937709E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.029740441505E+04 And the number of cells in the column are kmt = 5 Average salt = 3.47230031196141127E+01 Variance salt = 1.46447675703939240E-01 |dT/dt| salt = 2.04798368312225976E-01 Total salt = 4.64161515213081068E+19 yyyy/mm/dd hh:mm:ss = 1/ 1/19 0: 0: 0 The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.866130769344E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021144030582E+04 yyyy/mm/dd hh:mm:ss = 1/ 1/19 0: 0: 0 Tracer integrals for age_global And the number of cells in the column are kmt = 12 The maximum age_global is 4.916723706400E-02 yr at (i,j,k) = ( 338, 281, 4), (lon,lat,dpt) = ( 65.6026, 71.5268, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.693914597147E+04, 2.592186576923E+04, 9.845434069386E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.019022438636E+04 And the number of cells in the column are kmt = 9 Average age_global = 4.83696860390314815E-02 Variance age_global = 3.41861929295445878E-05 |dT/dt| age_global = 8.37389630256798606E-02 Total age_global = 6.46584245173646623E+19 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 1/19 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.64224830350689599E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -2.87711272348649816E+00 dbar Global max surface height on tracer cells (tau) = 1.04557961318387616E+00 m Global min surface height on tracer cells (tau) = -3.73071079463535327E+00 m Area average surface height on tracer cells (tau) = -1.69484166292173974E-03 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -6.12407309258589844E+11 m^3 Total Mass change = -2.32142425329537109E+12 kg Mass of ocean tracer cells (tau) = 1.33675510039881449E+21 kg Mass from sources = -6.86645507812500000E-05 kg Mass from eta smoothing = -6.86645507812500000E-05 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -5.24253085725898535E+12 kg Mass of river runoff liquid water input = 3.76436845434985042E+08 kg Mass of sea ice melt input = 2.92073016712499609E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = -6.81675231456756592E+00 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96570564700114228E+25 J Total heat change of full system for (taup1-taum1) = 5.14014503965994435E+19 J Total heat input to ocean referenced to 0degC = 5.14013659198979523E+19 J Heat input via surface heat fluxes = 5.15291005776326820E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -2.45667914636079232E+17 J Heat input via river runoff = 3.03971542457342422E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 1.17902859747106320E+17 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = 1.59236175781250000E+06 J Heat input via eta_t smooth = -1.60000000000000000E+01 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 5.14014503965994435E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 8.44766998988382500E+13 J Mismatch converted to a surface flux = 6.49416329668375949E-05 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161515213081068E+19 kg Total tracer change in system for (taup1-taum1) = 1.16829104050758057E+10 kg Total tracer input to ocean = 1.16829104292325993E+10 kg Tracer input via surface fluxes = 1.16829104292326050E+10 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = -8.68865442276000977E+00 kg Tracer input via eta_t smoother = -5.24520874023437500E-06 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 1.17397711300173092E+10 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = -1.55434226049485193E+01 kg Mismatch converted to a surface flux = -1.19490373921779487E-17 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 4.83696860390314815E-02 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066683925602848E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758072921745550E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758072921745591E-04 yr Age input via sources in th_tendency, or errors = 1.04307508496165581E-20 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.11905401502824565E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -1.85267141892098309E-06 yr Mismatch converted to a surface flux = -4.49457502196712211E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 455 idate: 10120 sec: 0 MATM istep1: 479 idate: 10121 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/21 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/21 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347840532624E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5832.2279 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347840532135E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.465014902850E+05 The minimum dzt is 4.764199052463E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 39.6644 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.764199051391E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.931275697572E+03 The minimum T is -2.098063442226E+00 deg C at (i,j,k) = ( 241, 2, 29), (lon,lat,dpt) = ( -39.5000, -77.6297, 812.7816 m) yyyy/mm/dd hh:mm:ss = 1/ 1/21 0: 0: 0 Tracer integrals for temp The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 5.025281930298E+01 m) The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.201151534820E+04 And the number of cells in the column are kmt = 29 The maximum T is 3.043129372741E+01 deg C at (i,j,k) = ( 49, 96, 4), (lon,lat,dpt) = ( -231.5000, -14.6898, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.075602990148E+05, 6.084705180670E+04, 1.013765756989E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.049131922580E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68365118520017631E+00 Variance temp = 2.01305333611995891E+01 |dT/dt| temp = 1.70070809747788831E+00 Total temp = 1.96576715597709344E+25 yyyy/mm/dd hh:mm:ss = 1/ 1/21 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/21 0: 0: 0 Tracer integrals for salt The maximum S is 4.059622760047E+01 psu at (i,j,k) = ( 332, 195, 1), (lon,lat,dpt) = ( 51.5000, 27.5082, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 1.003519337645E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.038648515658E+04 And the number of cells in the column are kmt = 5 The minimum S is 6.091705636514E+00 psu at (i,j,k) = ( 298, 237, 1), (lon,lat,dpt) = ( 17.5000, 60.9889, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.392724994408E+04, 5.550566181049E+04, 9.967662270573E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.031401158853E+04 And the number of cells in the column are kmt = 5 Average salt = 3.47230064563388652E+01 Variance salt = 1.46394707494437171E-01 |dT/dt| salt = 2.01406097590953126E-01 Total salt = 4.64161520864094945E+19 yyyy/mm/dd hh:mm:ss = 1/ 1/21 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/21 0: 0: 0 Tracer integrals for age_global The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.865442126750E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021072629560E+04 And the number of cells in the column are kmt = 12 The maximum age_global is 5.464293863957E-02 yr at (i,j,k) = ( 338, 281, 4), (lon,lat,dpt) = ( 65.6026, 71.5268, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.693914597147E+04, 2.592186576923E+04, 9.843914252484E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.018872483216E+04 And the number of cells in the column are kmt = 9 Average age_global = 5.37344014528704228E-02 Variance age_global = 4.32880454046451549E-05 |dT/dt| age_global = 8.43510943484273024E-02 Total age_global = 7.18297291809908326E+19 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 1/21 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.64524555610157552E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -2.82095580317350114E+00 dbar Global max surface height on tracer cells (tau) = 1.09743591874027890E+00 m Global min surface height on tracer cells (tau) = -3.70113331088199571E+00 m Area average surface height on tracer cells (tau) = -1.99480629388119326E-03 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -7.20795329530609375E+11 m^3 Total Mass change = -2.34419027504853516E+12 kg Mass of ocean tracer cells (tau) = 1.33675498821721365E+21 kg Mass from sources = 9.91821289062500000E-05 kg Mass from eta smoothing = 9.91821289062500000E-05 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -5.29797394354570703E+12 kg Mass of river runoff liquid water input = 3.77652838489167035E+08 kg Mass of sea ice melt input = 2.95340601532595752E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = 3.32725577533245087E+02 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96576715597709344E+25 J Total heat change of full system for (taup1-taum1) = 5.74479552895760794E+19 J Total heat input to ocean referenced to 0degC = 5.74478881405362668E+19 J Heat input via surface heat fluxes = 5.75837167350990930E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -2.29578198626619904E+17 J Heat input via river runoff = 3.07010175252418750E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 9.37189030462759360E+16 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = 1.16071212500000000E+06 J Heat input via eta_t smooth = -2.00000000000000000E+00 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 5.74479552895760794E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 6.71490386518958750E+13 J Mismatch converted to a surface flux = 5.16209585297422769E-05 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161520864094945E+19 kg Total tracer change in system for (taup1-taum1) = 1.18136137587026367E+10 kg Total tracer input to ocean = 1.18136137422840977E+10 kg Tracer input via surface fluxes = 1.18136137422841034E+10 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = 4.35620665550231934E+00 kg Tracer input via eta_t smoother = -5.48362731933593750E-06 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 1.18711106168662415E+10 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = 1.21210397634894846E+01 kg Mismatch converted to a surface flux = 9.31807369889698181E-18 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 5.37344014528704228E-02 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066675562983808E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758076214445810E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758076214445837E-04 yr Age input via sources in th_tendency, or errors = -4.16631020370776045E-21 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.11961253353560334E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -1.79682286088548064E-06 yr Mismatch converted to a surface flux = -4.35908659622919766E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 503 idate: 10122 sec: 0 MATM istep1: 527 idate: 10123 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/23 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/23 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347844311156E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5832.2345 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347844310668E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.465019278763E+05 The minimum dzt is 4.763407163380E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 39.6578 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.763407162309E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.929965046366E+03 The minimum T is -2.095934733943E+00 deg C at (i,j,k) = ( 241, 2, 29), (lon,lat,dpt) = ( -39.5000, -77.6297, 812.7816 m) yyyy/mm/dd hh:mm:ss = 1/ 1/23 0: 0: 0 Tracer integrals for temp The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 5.025406314776E+01 m) The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.201294707372E+04 And the number of cells in the column are kmt = 29 The maximum T is 3.047290228996E+01 deg C at (i,j,k) = ( 49, 96, 4), (lon,lat,dpt) = ( -231.5000, -14.6898, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.075602990148E+05, 6.084705180670E+04, 1.013796687340E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.049466567265E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68375993570993465E+00 Variance temp = 2.01331329650273751E+01 |dT/dt| temp = 1.68420175307625364E+00 Total temp = 1.96582502628503594E+25 yyyy/mm/dd hh:mm:ss = 1/ 1/23 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/23 0: 0: 0 Tracer integrals for salt The maximum S is 4.059228066494E+01 psu at (i,j,k) = ( 332, 195, 3), (lon,lat,dpt) = ( 51.5000, 27.5082, 25.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 1.004213203549E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.039280005095E+04 And the number of cells in the column are kmt = 5 The minimum S is 6.172355695890E+00 psu at (i,j,k) = ( 302, 236, 1), (lon,lat,dpt) = ( 21.5000, 60.4849, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.478054735269E+04, 5.660051823950E+04, 9.971072627169E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.032325987360E+04 And the number of cells in the column are kmt = 5 Average salt = 3.47230097802277982E+01 Variance salt = 1.46367657567452625E-01 |dT/dt| salt = 2.01843970660030847E-01 Total salt = 4.64161526571305533E+19 yyyy/mm/dd hh:mm:ss = 1/ 1/23 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/23 0: 0: 0 Tracer integrals for age_global The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.866701285888E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021197534231E+04 And the number of cells in the column are kmt = 12 The maximum age_global is 6.011864021514E-02 yr at (i,j,k) = ( 338, 281, 4), (lon,lat,dpt) = ( 65.6026, 71.5268, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.693914597147E+04, 2.592186576923E+04, 9.846165369064E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.019067562811E+04 And the number of cells in the column are kmt = 9 Average age_global = 5.90967425866661678E-02 Variance age_global = 5.35744844235800516E-05 |dT/dt| age_global = 8.51232173870740128E-02 Total age_global = 7.89978588493157171E+19 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 1/23 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.64146700386404998E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -2.74709298450136563E+00 dbar Global max surface height on tracer cells (tau) = 1.00787826047960349E+00 m Global min surface height on tracer cells (tau) = -3.67935271637301087E+00 m Area average surface height on tracer cells (tau) = -2.29301679634976449E-03 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -8.28549520028027344E+11 m^3 Total Mass change = -2.35127127445737793E+12 kg Mass of ocean tracer cells (tau) = 1.33675487669162633E+21 kg Mass from sources = 5.34057617187500000E-05 kg Mass from eta smoothing = 5.34057617187500000E-05 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -5.33501100178565234E+12 kg Mass of river runoff liquid water input = 3.83848144452653170E+08 kg Mass of sea ice melt input = 2.98335587924843311E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = -6.46109097003936768E+01 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96582502628503594E+25 J Total heat change of full system for (taup1-taum1) = 5.78846027453727867E+19 J Total heat input to ocean referenced to 0degC = 5.78845327200155648E+19 J Heat input via surface heat fluxes = 5.80951465629500539E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -3.08378377084512832E+17 J Heat input via river runoff = 3.11996239420412031E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 9.77333345260836480E+16 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = -5.87312031250000000E+04 J Heat input via eta_t smooth = 1.80000000000000000E+01 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 5.78846027453727867E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 7.00253572806192031E+13 J Mismatch converted to a surface flux = 5.38321342611086079E-05 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161526571305533E+19 kg Total tracer change in system for (taup1-taum1) = 1.19334132071292877E+10 kg Total tracer input to ocean = 1.19334132131089039E+10 kg Tracer input via surface fluxes = 1.19334132131089020E+10 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = -8.78335714340209961E+00 kg Tracer input via eta_t smoother = 1.43051147460937500E-06 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 1.19914931292083855E+10 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = 2.81738678558206557E+00 kg Mismatch converted to a surface flux = 2.16587175841376671E-18 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 5.90967425866661678E-02 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066668050940288E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758080086283746E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758080086283746E-04 yr Age input via sources in th_tendency, or errors = -4.15973562673107745E-21 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.11834347184306613E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -1.92373290197713225E-06 yr Mismatch converted to a surface flux = -4.66696995584812572E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 551 idate: 10124 sec: 0 MATM istep1: 575 idate: 10125 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/25 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/25 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347838202787E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5832.2239 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347838202298E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.465012754671E+05 The minimum dzt is 4.761574034949E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 39.6425 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.761574033877E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.927981163662E+03 The minimum T is -2.093699958387E+00 deg C at (i,j,k) = ( 241, 2, 29), (lon,lat,dpt) = ( -39.5000, -77.6297, 812.7816 m) yyyy/mm/dd hh:mm:ss = 1/ 1/25 0: 0: 0 Tracer integrals for temp The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 5.025455138014E+01 m) The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.201350669032E+04 And the number of cells in the column are kmt = 29 The maximum T is 3.050587112369E+01 deg C at (i,j,k) = ( 49, 96, 4), (lon,lat,dpt) = ( -231.5000, -14.6898, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.075602990148E+05, 6.084705180670E+04, 1.013883544840E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.049313428984E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68390393989350518E+00 Variance temp = 2.01368209550858097E+01 |dT/dt| temp = 1.70253157649968956E+00 Total temp = 1.96590170707328322E+25 yyyy/mm/dd hh:mm:ss = 1/ 1/25 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/25 0: 0: 0 Tracer integrals for salt The maximum S is 4.058521166049E+01 psu at (i,j,k) = ( 332, 195, 3), (lon,lat,dpt) = ( 51.5000, 27.5082, 25.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 1.004499862363E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.039828895779E+04 And the number of cells in the column are kmt = 5 The minimum S is 6.188686052839E+00 psu at (i,j,k) = ( 302, 236, 2), (lon,lat,dpt) = ( 21.5000, 60.4849, 15.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.478054735269E+04, 5.660051823950E+04, 1.004501295055E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.039392805452E+04 And the number of cells in the column are kmt = 5 Average salt = 3.47230131500594439E+01 Variance salt = 1.46338481175234847E-01 |dT/dt| salt = 1.98420352989349957E-01 Total salt = 4.64161532301764116E+19 yyyy/mm/dd hh:mm:ss = 1/ 1/25 0: 0: 0 The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.868084746306E+00 m) yyyy/mm/dd hh:mm:ss = 1/ 1/25 0: 0: 0 Tracer integrals for age_global The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021353461559E+04 And the number of cells in the column are kmt = 12 The maximum age_global is 6.559434179072E-02 yr at (i,j,k) = ( 338, 281, 4), (lon,lat,dpt) = ( 65.6026, 71.5268, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.693914597147E+04, 2.592186576923E+04, 9.837940596309E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.018185003279E+04 And the number of cells in the column are kmt = 9 Average age_global = 6.44580512249475768E-02 Variance age_global = 6.50566225603053591E-05 |dT/dt| age_global = 8.59283451606270010E-02 Total age_global = 8.61646070185762488E+19 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 1/25 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.63453713842816661E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -2.66115272901449362E+00 dbar Global max surface height on tracer cells (tau) = 1.03219046715367213E+00 m Global min surface height on tracer cells (tau) = -3.65389786263560934E+00 m Area average surface height on tracer cells (tau) = -2.59577754189144541E-03 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -9.37947877162269531E+11 m^3 Total Mass change = -2.33286382825603906E+12 kg Mass of ocean tracer cells (tau) = 1.33675476346432677E+21 kg Mass from sources = 1.29699707031250000E-04 kg Mass from eta smoothing = 1.29699707031250000E-04 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -5.29543393500402832E+12 kg Mass of river runoff liquid water input = 3.94140836206926703E+08 kg Mass of sea ice melt input = 2.96217596503672559E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = 8.75056615471839905E+02 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96590170707328322E+25 J Total heat change of full system for (taup1-taum1) = 6.36203012854081454E+19 J Total heat input to ocean referenced to 0degC = 6.36202199607563878E+19 J Heat input via surface heat fluxes = 6.37765953843055985E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -2.69910898174282560E+17 J Heat input via river runoff = 3.18862962926105977E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 1.13503588328779456E+17 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = 1.49050340234375000E+06 J Heat input via eta_t smooth = -1.00000000000000000E+01 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 6.36203012854081454E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 8.13246502670645937E+13 J Mismatch converted to a surface flux = 6.25184884722606194E-05 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161532301764116E+19 kg Total tracer change in system for (taup1-taum1) = 1.18486937020596924E+10 kg Total tracer input to ocean = 1.18486936853208046E+10 kg Tracer input via surface fluxes = 1.18486936853208008E+10 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = 1.86913681030273438E+00 kg Tracer input via eta_t smoother = 3.81469726562500000E-06 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 1.19063612943076172E+10 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = 1.49421220545654290E+01 kg Mismatch converted to a surface flux = 1.14867863845924453E-17 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 6.44580512249475768E-02 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066654919213440E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758079896794547E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758079896794561E-04 yr Age input via sources in th_tendency, or errors = 6.96576792411683158E-21 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.11847151829493573E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -1.91092806730097288E-06 yr Mismatch converted to a surface flux = -4.63590546728954303E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 599 idate: 10126 sec: 0 MATM istep1: 623 idate: 10127 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/27 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/27 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347836599387E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5832.2211 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347836598898E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.465010819128E+05 The minimum dzt is 4.766327936278E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 39.6821 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.766327935205E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.933555760583E+03 The minimum T is -2.091380906554E+00 deg C at (i,j,k) = ( 241, 2, 29), (lon,lat,dpt) = ( -39.5000, -77.6297, 812.7816 m) yyyy/mm/dd hh:mm:ss = 1/ 1/27 0: 0: 0 Tracer integrals for temp The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 5.025545103600E+01 m) The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.201428933508E+04 And the number of cells in the column are kmt = 29 The maximum T is 3.048941233251E+01 deg C at (i,j,k) = ( 49, 96, 4), (lon,lat,dpt) = ( -231.5000, -14.6898, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.075602990148E+05, 6.084705180670E+04, 1.013984239014E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.049552098596E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68407488462301291E+00 Variance temp = 2.01415454708528969E+01 |dT/dt| temp = 1.68983835219464229E+00 Total temp = 1.96599277377749859E+25 yyyy/mm/dd hh:mm:ss = 1/ 1/27 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/27 0: 0: 0 Tracer integrals for salt The maximum S is 4.058535059958E+01 psu at (i,j,k) = ( 332, 195, 4), (lon,lat,dpt) = ( 51.5000, 27.5082, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 1.004054404284E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.039194225485E+04 And the number of cells in the column are kmt = 5 The minimum S is 6.206376697959E+00 psu at (i,j,k) = ( 302, 236, 2), (lon,lat,dpt) = ( 21.5000, 60.4849, 15.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.478054735269E+04, 5.660051823950E+04, 1.000012211604E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.035420195610E+04 And the number of cells in the column are kmt = 5 Average salt = 3.47230163332440327E+01 Variance salt = 1.46304913542053328E-01 |dT/dt| salt = 1.96081759534192934E-01 Total salt = 4.64161537711059681E+19 yyyy/mm/dd hh:mm:ss = 1/ 1/27 0: 0: 0 The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.866814522520E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021210077270E+04 yyyy/mm/dd hh:mm:ss = 1/ 1/27 0: 0: 0 Tracer integrals for age_global And the number of cells in the column are kmt = 12 The maximum age_global is 7.107004336629E-02 yr at (i,j,k) = ( 338, 281, 4), (lon,lat,dpt) = ( 65.6026, 71.5268, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.693914597147E+04, 2.592186576923E+04, 9.843016815449E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.018766486934E+04 And the number of cells in the column are kmt = 9 Average age_global = 6.98195271551343699E-02 Variance age_global = 7.75731815471263422E-05 |dT/dt| age_global = 8.65923273608041333E-02 Total age_global = 9.33315780390860882E+19 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 1/27 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.62989156612679364E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -2.62230277967145664E+00 dbar Global max surface height on tracer cells (tau) = 1.07391873601728549E+00 m Global min surface height on tracer cells (tau) = -3.67680320407543082E+00 m Area average surface height on tracer cells (tau) = -2.88179803256934054E-03 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -1.04129737754386328E+12 m^3 Total Mass change = -2.24467442311507910E+12 kg Mass of ocean tracer cells (tau) = 1.33675465649759401E+21 kg Mass from sources = -1.18255615234375000E-04 kg Mass from eta smoothing = -1.18255615234375000E-04 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -5.08849537307186133E+12 kg Mass of river runoff liquid water input = 4.03556080206377149E+08 kg Mass of sea ice melt input = 2.84341739420563232E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = -3.29055868268013000E+02 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96599277377749859E+25 J Total heat change of full system for (taup1-taum1) = 6.12559070828284314E+19 J Total heat input to ocean referenced to 0degC = 6.12558428731459174E+19 J Heat input via surface heat fluxes = 6.14679257321541878E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -3.01731745738271872E+17 J Heat input via river runoff = 3.23992702404923867E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 8.96164874597585920E+16 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = 2.78414761328125000E+06 J Heat input via eta_t smooth = 0.00000000000000000E+00 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 6.12559070828284314E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 6.42096797297723906E+13 J Mismatch converted to a surface flux = 4.93613204460229582E-05 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161537711059681E+19 kg Total tracer change in system for (taup1-taum1) = 1.13736595152633667E+10 kg Total tracer input to ocean = 1.13736595180132732E+10 kg Tracer input via surface fluxes = 1.13736595180132751E+10 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = -4.01202178001403809E+00 kg Tracer input via eta_t smoother = -2.14576721191406250E-06 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 1.14290151161241531E+10 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = 1.26825795497059812E+00 kg Mismatch converted to a surface flux = 9.74975853905312086E-19 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 6.98195271551343699E-02 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066641917794528E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758079266072199E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758079266072172E-04 yr Age input via sources in th_tendency, or errors = -2.56129882481201962E-20 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.11781738341135470E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -1.97634092493672002E-06 yr Mismatch converted to a surface flux = -4.79459685370729817E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 647 idate: 10128 sec: 0 MATM istep1: 671 idate: 10129 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/29 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/29 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347840162657E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5832.2273 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347840162168E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.465014765251E+05 The minimum dzt is 4.773022339037E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 39.7379 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.773022337963E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.939331337065E+03 The minimum T is -2.089002264846E+00 deg C at (i,j,k) = ( 241, 2, 29), (lon,lat,dpt) = ( -39.5000, -77.6297, 812.7816 m) yyyy/mm/dd hh:mm:ss = 1/ 1/29 0: 0: 0 Tracer integrals for temp The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 5.025466061591E+01 m) The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.201371299233E+04 And the number of cells in the column are kmt = 29 The maximum T is 3.044501407134E+01 deg C at (i,j,k) = ( 49, 96, 4), (lon,lat,dpt) = ( -231.5000, -14.6898, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.075602990148E+05, 6.084705180670E+04, 1.014596549920E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.050164208496E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68419604342282136E+00 Variance temp = 2.01455554397305896E+01 |dT/dt| temp = 1.71194390423753706E+00 Total temp = 1.96605726421630278E+25 yyyy/mm/dd hh:mm:ss = 1/ 1/29 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/29 0: 0: 0 Tracer integrals for salt The maximum S is 4.058522419134E+01 psu at (i,j,k) = ( 332, 195, 2), (lon,lat,dpt) = ( 51.5000, 27.5082, 15.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 1.005015424526E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.040251512584E+04 And the number of cells in the column are kmt = 5 The minimum S is 6.226280882284E+00 psu at (i,j,k) = ( 302, 236, 1), (lon,lat,dpt) = ( 21.5000, 60.4849, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.478054735269E+04, 5.660051823950E+04, 9.996377866663E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.034590978704E+04 And the number of cells in the column are kmt = 5 Average salt = 3.47230196877423296E+01 Variance salt = 1.46271954219400868E-01 |dT/dt| salt = 1.94756811470690405E-01 Total salt = 4.64161543479695114E+19 yyyy/mm/dd hh:mm:ss = 1/ 1/29 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/29 0: 0: 0 Tracer integrals for age_global The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.868000476821E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021326395710E+04 And the number of cells in the column are kmt = 12 The maximum age_global is 7.654574494186E-02 yr at (i,j,k) = ( 338, 281, 5), (lon,lat,dpt) = ( 65.6026, 71.5268, 45.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.693914597147E+04, 2.592186576923E+04, 9.849324301322E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.019411478251E+04 And the number of cells in the column are kmt = 9 Average age_global = 7.51729542273237572E-02 Variance age_global = 9.17757377873525820E-05 |dT/dt| age_global = 8.72973915067885853E-02 Total age_global = 1.00487788147067535E+20 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 1/29 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.64030336953550582E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -2.55786489458736055E+00 dbar Global max surface height on tracer cells (tau) = 1.23245803342116544E+00 m Global min surface height on tracer cells (tau) = -3.66641054681356016E+00 m Area average surface height on tracer cells (tau) = -3.18268626633436700E-03 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -1.15001912876040625E+12 m^3 Total Mass change = -2.36709414501636914E+12 kg Mass of ocean tracer cells (tau) = 1.33675454397058122E+21 kg Mass from sources = 1.83105468750000000E-04 kg Mass from eta smoothing = 1.83105468750000000E-04 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -5.42331372121805078E+12 kg Mass of river runoff liquid water input = 4.27711022284916162E+08 kg Mass of sea ice melt input = 3.05579186509437256E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = 8.50234944820404053E+01 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96605726421630278E+25 J Total heat change of full system for (taup1-taum1) = 6.46349438715801518E+19 J Total heat input to ocean referenced to 0degC = 6.46348878052434002E+19 J Heat input via surface heat fluxes = 6.46910893815432970E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -1.34485199983438656E+17 J Heat input via river runoff = 3.26760972753647266E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 7.82509475862602880E+16 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = -1.29500072656250000E+06 J Heat input via eta_t smooth = -1.20000000000000000E+01 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 6.46349438715801518E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 5.60663380466167266E+13 J Mismatch converted to a surface flux = 4.31011101472738561E-05 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161543479695114E+19 kg Total tracer change in system for (taup1-taum1) = 1.22231573700388184E+10 kg Total tracer input to ocean = 1.22231573756042767E+10 kg Tracer input via surface fluxes = 1.22231573756042786E+10 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = 4.60835695266723633E-02 kg Tracer input via eta_t smoother = -2.02655792236328125E-06 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 1.22826474769587975E+10 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = -5.63885324152410039E+00 kg Mismatch converted to a surface flux = -4.33487977162276158E-18 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 7.51729542273237572E-02 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066627256548352E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758077884769127E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758077884769100E-04 yr Age input via sources in th_tendency, or errors = 8.43051652286273414E-21 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.11716812656843768E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -2.04126522792535513E-06 yr Mismatch converted to a surface flux = -4.95210300809127183E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 695 idate: 10130 sec: 0 MATM istep1: 719 idate: 10131 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/31 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/31 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347837390375E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5832.2224 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347837389887E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.465012068285E+05 The minimum dzt is 4.771898408832E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 39.7285 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.771898407759E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.939322965618E+03 The minimum T is -2.086586483741E+00 deg C at (i,j,k) = ( 241, 2, 29), (lon,lat,dpt) = ( -39.5000, -77.6297, 812.7816 m) yyyy/mm/dd hh:mm:ss = 1/ 1/31 0: 0: 0 Tracer integrals for temp The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 5.025425964935E+01 m) The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.201315400347E+04 And the number of cells in the column are kmt = 29 The maximum T is 3.046365088420E+01 deg C at (i,j,k) = ( 49, 96, 1), (lon,lat,dpt) = ( -231.5000, -14.6898, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.075602990148E+05, 6.084705180670E+04, 1.015059889005E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.050542688624E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68434814019334222E+00 Variance temp = 2.01498036351477836E+01 |dT/dt| temp = 1.66759836560294916E+00 Total temp = 1.96613826448819455E+25 yyyy/mm/dd hh:mm:ss = 1/ 1/31 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/31 0: 0: 0 Tracer integrals for salt The maximum S is 4.057743171380E+01 psu at (i,j,k) = ( 332, 195, 3), (lon,lat,dpt) = ( 51.5000, 27.5082, 25.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 1.006177907740E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.041458944672E+04 And the number of cells in the column are kmt = 5 The minimum S is 6.244355925435E+00 psu at (i,j,k) = ( 302, 236, 1), (lon,lat,dpt) = ( 21.5000, 60.4849, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.478054735269E+04, 5.660051823950E+04, 1.000362058240E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.034987350995E+04 And the number of cells in the column are kmt = 5 Average salt = 3.47230230402943434E+01 Variance salt = 1.46240104799289838E-01 |dT/dt| salt = 1.87834800775930982E-01 Total salt = 4.64161549202114970E+19 yyyy/mm/dd hh:mm:ss = 1/ 1/31 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 1/31 0: 0: 0 Tracer integrals for age_global The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.866290485103E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021155874710E+04 And the number of cells in the column are kmt = 12 The maximum age_global is 8.202144651744E-02 yr at (i,j,k) = ( 338, 281, 5), (lon,lat,dpt) = ( 65.6026, 71.5268, 45.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.693914597147E+04, 2.592186576923E+04, 9.840883616685E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.018586675134E+04 And the number of cells in the column are kmt = 9 Average age_global = 8.05253826759229491E-02 Variance age_global = 1.07251518518953516E-04 |dT/dt| age_global = 8.78943104461942792E-02 Total age_global = 1.07642662131046728E+20 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 1/31 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.65648351092673840E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -2.53081228391015900E+00 dbar Global max surface height on tracer cells (tau) = 1.35659628951467592E+00 m Global min surface height on tracer cells (tau) = -3.66756630242563109E+00 m Area average surface height on tracer cells (tau) = -3.48372998582598126E-03 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -1.25879706256764844E+12 m^3 Total Mass change = -2.31219090405091797E+12 kg Mass of ocean tracer cells (tau) = 1.33675443138541991E+21 kg Mass from sources = -4.95910644531250000E-05 kg Mass from eta smoothing = -4.95910644531250000E-05 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -5.25406973332323340E+12 kg Mass of river runoff liquid water input = 4.50775331558878958E+08 kg Mass of sea ice melt input = 2.94142805415102734E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = -2.10270743429660797E+02 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96613826448819455E+25 J Total heat change of full system for (taup1-taum1) = 6.63211587952851354E+19 J Total heat input to ocean referenced to 0degC = 6.63211052628772045E+19 J Heat input via surface heat fluxes = 6.65359962365281649E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -2.89638117592594560E+17 J Heat input via river runoff = 3.27749813617487773E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 7.47143689602731200E+16 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = -1.97858777343750000E+05 J Heat input via eta_t smooth = 1.40000000000000000E+01 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 6.63211587952851354E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 5.35324081287387812E+13 J Mismatch converted to a surface flux = 4.11531464260634169E-05 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161549202114970E+19 kg Total tracer change in system for (taup1-taum1) = 1.17657021766176758E+10 kg Total tracer input to ocean = 1.17657021565138664E+10 kg Tracer input via surface fluxes = 1.17657021565138702E+10 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = 6.73736906051635742E+00 kg Tracer input via eta_t smoother = -3.33786010742187500E-06 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 1.18229658491112728E+10 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = 1.34314947610945694E+01 kg Mismatch converted to a surface flux = 1.03254886142042712E-17 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 8.05253826759229491E-02 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066608029495840E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758073077733173E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758073077733186E-04 yr Age input via sources in th_tendency, or errors = -1.12182861891819462E-20 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.11687907763303209E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -2.07016531442995505E-06 yr Mismatch converted to a surface flux = -5.02221452684720719E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 743 idate: 10201 sec: 0 MATM istep1: 767 idate: 10202 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/ 2 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/ 2 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347842417467E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5832.2312 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347842416978E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.465017170446E+05 The minimum dzt is 4.764219678850E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 39.6646 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.764219677778E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.930920076630E+03 yyyy/mm/dd hh:mm:ss = 1/ 2/ 2 0: 0: 0 Tracer integrals for temp The minimum T is -2.084158989579E+00 deg C at (i,j,k) = ( 241, 2, 29), (lon,lat,dpt) = ( -39.5000, -77.6297, 812.7816 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 5.025705388544E+01 m) The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.201606926560E+04 And the number of cells in the column are kmt = 29 The maximum T is 3.050640662750E+01 deg C at (i,j,k) = ( 60, 92, 2), (lon,lat,dpt) = ( -220.5000, -17.1490, 15.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.062513287499E+05, 7.606978203305E+04, 1.016297219166E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.051766422244E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68454134986229320E+00 Variance temp = 2.01552189292882780E+01 |dT/dt| temp = 1.69789246972430519E+00 Total temp = 1.96624120228222019E+25 yyyy/mm/dd hh:mm:ss = 1/ 2/ 2 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/ 2 0: 0: 0 Tracer integrals for salt The maximum S is 4.057161577942E+01 psu at (i,j,k) = ( 332, 195, 1), (lon,lat,dpt) = ( 51.5000, 27.5082, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 1.005853024987E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.041050147729E+04 And the number of cells in the column are kmt = 5 The minimum S is 6.260609750618E+00 psu at (i,j,k) = ( 302, 236, 1), (lon,lat,dpt) = ( 21.5000, 60.4849, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.478054735269E+04, 5.660051823950E+04, 1.008017739175E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.043673009977E+04 And the number of cells in the column are kmt = 5 Average salt = 3.47230264377997031E+01 Variance salt = 1.46215046804400117E-01 |dT/dt| salt = 1.86414882163130735E-01 Total salt = 4.64161555005385196E+19 yyyy/mm/dd hh:mm:ss = 1/ 2/ 2 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/ 2 0: 0: 0 Tracer integrals for age_global The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.867265865053E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021244720963E+04 And the number of cells in the column are kmt = 12 The maximum age_global is 8.749714809301E-02 yr at (i,j,k) = ( 338, 281, 5), (lon,lat,dpt) = ( 65.6026, 71.5268, 45.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.693914597147E+04, 2.592186576923E+04, 9.830177549055E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.017405019941E+04 And the number of cells in the column are kmt = 9 Average age_global = 8.58766892700637691E-02 Variance age_global = 1.23965264437865021E-04 |dT/dt| age_global = 8.89373237983167031E-02 Total age_global = 1.14796035137405288E+20 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 2/ 2 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.65222535794116565E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -2.49619129805648710E+00 dbar Global max surface height on tracer cells (tau) = 1.08068757083165834E+00 m Global min surface height on tracer cells (tau) = -3.63626848186354623E+00 m Area average surface height on tracer cells (tau) = -3.78877852049074168E-03 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -1.36902208027536328E+12 m^3 Total Mass change = -2.35601158824571094E+12 kg Mass of ocean tracer cells (tau) = 1.33675431730252638E+21 kg Mass from sources = -5.72204589843750000E-05 kg Mass from eta smoothing = -5.72204589843750000E-05 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -5.35721569682346484E+12 kg Mass of river runoff liquid water input = 4.98195378609057307E+08 kg Mass of sea ice melt input = 3.00070591350617676E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = -3.07031851649284363E+02 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96624120228222019E+25 J Total heat change of full system for (taup1-taum1) = 7.24749723947323802E+19 J Total heat input to ocean referenced to 0degC = 7.24749274761364603E+19 J Heat input via surface heat fluxes = 7.26397000805277204E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -2.27498882280281856E+17 J Heat input via river runoff = 3.40681621796161445E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 6.26922097268369840E+16 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = -2.74101214453125000E+06 J Heat input via eta_t smooth = -1.20000000000000000E+01 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 7.24749723947323802E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 4.49185986608841406E+13 J Mismatch converted to a surface flux = 3.45312630715104090E-05 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161555005385196E+19 kg Total tracer change in system for (taup1-taum1) = 1.20028135248403320E+10 kg Total tracer input to ocean = 1.20028135394204388E+10 kg Tracer input via surface fluxes = 1.20028135394204407E+10 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = -2.60244476795196533E+00 kg Tracer input via eta_t smoother = -2.74181365966796875E-06 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 1.20612312182657299E+10 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = -1.20359572480722665E+01 kg Mismatch converted to a surface flux = -9.25266634403183008E-18 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 8.58766892700637691E-02 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066598822370880E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758075902268741E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758075902268754E-04 yr Age input via sources in th_tendency, or errors = -1.36349382202886455E-20 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.11725664670994315E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -2.03241123127442003E-06 yr Mismatch converted to a surface flux = -4.93062324012731709E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 791 idate: 10203 sec: 0 MATM istep1: 815 idate: 10204 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/ 4 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/ 4 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347839178780E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5832.2256 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347839178291E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.465013589685E+05 The minimum dzt is 4.760824301813E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 39.6363 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.760824300742E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.927539987389E+03 The minimum T is -2.081730586966E+00 deg C at (i,j,k) = ( 241, 2, 29), (lon,lat,dpt) = ( -39.5000, -77.6297, 812.7816 m) yyyy/mm/dd hh:mm:ss = 1/ 2/ 4 0: 0: 0 Tracer integrals for temp The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 5.025638873309E+01 m) The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.201540068726E+04 And the number of cells in the column are kmt = 29 The maximum T is 3.056249499487E+01 deg C at (i,j,k) = ( 60, 92, 4), (lon,lat,dpt) = ( -220.5000, -17.1490, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.062513287499E+05, 7.606978203305E+04, 1.017124081953E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.052703392921E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68476328855611257E+00 Variance temp = 2.01622693926804324E+01 |dT/dt| temp = 1.60792228843871632E+00 Total temp = 1.96635946969053967E+25 yyyy/mm/dd hh:mm:ss = 1/ 2/ 4 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/ 4 0: 0: 0 Tracer integrals for salt The maximum S is 4.056969225320E+01 psu at (i,j,k) = ( 332, 195, 2), (lon,lat,dpt) = ( 51.5000, 27.5082, 15.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 1.002951896390E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.038210122676E+04 And the number of cells in the column are kmt = 5 The minimum S is 6.283168269328E+00 psu at (i,j,k) = ( 302, 236, 1), (lon,lat,dpt) = ( 21.5000, 60.4849, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.478054735269E+04, 5.660051823950E+04, 1.002488960326E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.037311861093E+04 And the number of cells in the column are kmt = 5 Average salt = 3.47230298630297654E+01 Variance salt = 1.46186079758081178E-01 |dT/dt| salt = 1.82168743659563176E-01 Total salt = 4.64161560825298452E+19 yyyy/mm/dd hh:mm:ss = 1/ 2/ 4 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/ 4 0: 0: 0 Tracer integrals for age_global The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.867936708629E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021336063231E+04 And the number of cells in the column are kmt = 12 The maximum age_global is 9.297284966858E-02 yr at (i,j,k) = ( 338, 281, 5), (lon,lat,dpt) = ( 65.6026, 71.5268, 45.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.693914597147E+04, 2.592186576923E+04, 9.832174686443E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.017617933313E+04 And the number of cells in the column are kmt = 9 Average age_global = 9.12324161872050815E-02 Variance age_global = 1.41171550432531850E-04 |dT/dt| age_global = 8.91023662973555730E-02 Total age_global = 1.21955315715128574E+20 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 2/ 4 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.64973145944289867E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -2.46944793511182104E+00 dbar Global max surface height on tracer cells (tau) = 1.11654174753723545E+00 m Global min surface height on tracer cells (tau) = -3.65439821352463179E+00 m Area average surface height on tracer cells (tau) = -4.09655280190997142E-03 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -1.48023200841580078E+12 m^3 Total Mass change = -2.43297423517167480E+12 kg Mass of ocean tracer cells (tau) = 1.33675420220025078E+21 kg Mass from sources = -3.05175781250000000E-05 kg Mass from eta smoothing = -3.05175781250000000E-05 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -5.52765536391353711E+12 kg Mass of river runoff liquid water input = 5.19208754306821346E+08 kg Mass of sea ice melt input = 3.09416191851406055E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = 1.47349496698379517E+03 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96635946969053967E+25 J Total heat change of full system for (taup1-taum1) = 6.70600169031186924E+19 J Total heat input to ocean referenced to 0degC = 6.70599698085284577E+19 J Heat input via surface heat fluxes = 6.72319580595432325E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -2.37752225135537344E+17 J Heat input via river runoff = 3.47651338147749180E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 6.57292089869403040E+16 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = -1.45388691796875000E+06 J Heat input via eta_t smooth = 8.00000000000000000E+00 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 6.70600169031186924E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 4.70945916885109219E+13 J Mismatch converted to a surface flux = 3.62040620883725641E-05 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161560825298452E+19 kg Total tracer change in system for (taup1-taum1) = 1.23766376328572083E+10 kg Total tracer input to ocean = 1.23766376132151604E+10 kg Tracer input via surface fluxes = 1.23766376132151642E+10 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = -5.24424386024475098E+00 kg Tracer input via eta_t smoother = -3.57627868652343750E-06 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 1.24368747282163239E+10 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = 2.50074133242347223E+01 kg Mismatch converted to a surface flux = 1.92244992938554575E-17 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 9.12324161872050815E-02 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066590008653632E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758079110675534E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758079110675507E-04 yr Age input via sources in th_tendency, or errors = -5.44579362553516708E-20 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.11796402966801269E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -1.96167614387426480E-06 yr Mismatch converted to a surface flux = -4.75902014107882992E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 839 idate: 10205 sec: 0 MATM istep1: 863 idate: 10206 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/ 6 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/ 6 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347845402760E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5832.2364 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347845402271E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.465020079449E+05 The minimum dzt is 4.768497518988E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 39.7002 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.768497517915E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.935514503145E+03 yyyy/mm/dd hh:mm:ss = 1/ 2/ 6 0: 0: 0 Tracer integrals for temp The minimum T is -2.079302647968E+00 deg C at (i,j,k) = ( 241, 2, 29), (lon,lat,dpt) = ( -39.5000, -77.6297, 812.7816 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 5.025540489618E+01 m) The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.201443172725E+04 And the number of cells in the column are kmt = 29 The maximum T is 3.061029406408E+01 deg C at (i,j,k) = ( 60, 92, 4), (lon,lat,dpt) = ( -220.5000, -17.1490, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.062513287499E+05, 7.606978203305E+04, 1.015640844540E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.051252511258E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68491550701911663E+00 Variance temp = 2.01676963034243002E+01 |dT/dt| temp = 1.62825633303766981E+00 Total temp = 1.96644052747686980E+25 yyyy/mm/dd hh:mm:ss = 1/ 2/ 6 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/ 6 0: 0: 0 Tracer integrals for salt The maximum S is 4.057054517469E+01 psu at (i,j,k) = ( 332, 195, 2), (lon,lat,dpt) = ( 51.5000, 27.5082, 15.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 1.001058445964E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.036145521387E+04 And the number of cells in the column are kmt = 5 The minimum S is 6.299760556817E+00 psu at (i,j,k) = ( 302, 236, 1), (lon,lat,dpt) = ( 21.5000, 60.4849, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.478054735269E+04, 5.660051823950E+04, 9.994447690087E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.034309509515E+04 And the number of cells in the column are kmt = 5 Average salt = 3.47230333650074598E+01 Variance salt = 1.46155307607386931E-01 |dT/dt| salt = 1.83942194808080495E-01 Total salt = 4.64161566803157156E+19 yyyy/mm/dd hh:mm:ss = 1/ 2/ 6 0: 0: 0 The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.868377266115E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021359219776E+04 yyyy/mm/dd hh:mm:ss = 1/ 2/ 6 0: 0: 0 Tracer integrals for age_global And the number of cells in the column are kmt = 12 Average age_global = 9.65839525567570162E-02 Variance age_global = 1.59842985764407919E-04 |dT/dt| age_global = 9.08539653144073145E-02 Total age_global = 1.29108993086890410E+20 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 2/ 6 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.67107934251688439E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -2.43659611830385403E+00 dbar Global max surface height on tracer cells (tau) = 1.00005416735488351E+00 m Global min surface height on tracer cells (tau) = -3.67688270923770233E+00 m Area average surface height on tracer cells (tau) = -4.41101109650300378E-03 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -1.59385711114886743E+12 m^3 Total Mass change = -2.38538284488712305E+12 kg Mass of ocean tracer cells (tau) = 1.33675408459826935E+21 kg Mass from sources = -1.75476074218750000E-04 kg Mass from eta smoothing = -1.75476074218750000E-04 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -5.45161056610140527E+12 kg Mass of river runoff liquid water input = 5.32257385955607057E+08 kg Mass of sea ice melt input = 3.06569546389392236E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = -6.55950800180435181E+01 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96644052747686980E+25 J Total heat change of full system for (taup1-taum1) = 5.73316468374793667E+19 J Total heat input to ocean referenced to 0degC = 5.73315748329048965E+19 J Heat input via surface heat fluxes = 5.74842696598295020E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -2.53225942343138208E+17 J Heat input via river runoff = 3.54274750291691797E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 1.00495687943507040E+17 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = 3.21266820312500000E+05 J Heat input via eta_t smooth = -4.00000000000000000E+00 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 5.73316468374793667E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 7.20045741488771875E+13 J Mismatch converted to a surface flux = 5.53536612096530465E-05 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161566803157156E+19 kg Total tracer change in system for (taup1-taum1) = 1.22627719081523438E+10 kg Total tracer input to ocean = 1.22627718893260021E+10 kg Tracer input via surface fluxes = 1.22627718893260040E+10 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+0 The maximum age_global is 9.844855124415E-02 yr at (i,j,k) = ( 338, 281, 5), (lon,lat,dpt) = ( 65.6026, 71.5268, 45.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.693914597147E+04, 2.592186576923E+04, 9.833235907106E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.017760058255E+04 And the number of cells in the column are kmt = 9 0 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = 3.87819051742553711E-01 kg Tracer input via eta_t smoother = -1.66893005371093750E-06 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 1.23224548190293198E+10 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = 1.85282628666694151E+01 kg Mismatch converted to a surface flux = 1.42436393471956507E-17 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 9.65839525567570162E-02 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066587095230560E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758086935105386E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758086935105413E-04 yr Age input via sources in th_tendency, or errors = -1.53911770487665698E-20 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.11619154717803364E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -2.13893221730202002E-06 yr Mismatch converted to a surface flux = -5.18904281643502436E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 887 idate: 10207 sec: 0 MATM istep1: 911 idate: 10208 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/ 8 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/ 8 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347840456350E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5832.2278 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347840455861E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.465014819059E+05 The minimum dzt is 4.759371818118E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 39.6242 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.759371817047E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.925904418820E+03 The minimum T is -2.076864202049E+00 deg C at (i,j,k) = ( 241, 2, 29), (lon,lat,dpt) = ( -39.5000, -77.6297, 812.7816 m) yyyy/mm/dd hh:mm:ss = 1/ 2/ 8 0: 0: 0 Tracer integrals for temp The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 5.025568299998E+01 m) The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.201461122243E+04 And the number of cells in the column are kmt = 29 The maximum T is 3.057678208776E+01 deg C at (i,j,k) = ( 60, 92, 4), (lon,lat,dpt) = ( -220.5000, -17.1490, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.062513287499E+05, 7.606978203305E+04, 1.016633116636E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.052266968506E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68506559685679891E+00 Variance temp = 2.01733048089019462E+01 |dT/dt| temp = 1.55855791892365669E+00 Total temp = 1.96652045533584426E+25 yyyy/mm/dd hh:mm:ss = 1/ 2/ 8 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/ 8 0: 0: 0 Tracer integrals for salt The maximum S is 4.058023123299E+01 psu at (i,j,k) = ( 332, 195, 5), (lon,lat,dpt) = ( 51.5000, 27.5082, 45.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 9.960132143213E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.031218702232E+04 And the number of cells in the column are kmt = 5 The minimum S is 6.318463538221E+00 psu at (i,j,k) = ( 302, 236, 1), (lon,lat,dpt) = ( 21.5000, 60.4849, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.478054735269E+04, 5.660051823950E+04, 9.948739699769E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.029809452057E+04 And the number of cells in the column are kmt = 5 Average salt = 3.47230367495804870E+01 Variance salt = 1.46118550316032270E-01 |dT/dt| salt = 1.78944228625767143E-01 Total salt = 4.64161572632339907E+19 yyyy/mm/dd hh:mm:ss = 1/ 2/ 8 0: 0: 0 The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.868649033406E+00 m) yyyy/mm/dd hh:mm:ss = 1/ 2/ 8 0: 0: 0 Tracer integrals for age_global The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021395933365E+04 And the number of cells in the column are kmt = 12 The maximum age_global is 1.039242528197E-01 yr at (i,j,k) = ( 338, 281, 5), (lon,lat,dpt) = ( 65.6026, 71.5268, 45.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.693914597147E+04, 2.592186576923E+04, 9.829750015201E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.017354532523E+04 And the number of cells in the column are kmt = 9 Average age_global = 1.01933036591015186E-01 Variance age_global = 1.79861506771475388E-04 |dT/dt| age_global = 9.08194397847503776E-02 Total age_global = 1.36259391448091263E+20 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 2/ 8 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.67492064419724063E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -2.38761712479395793E+00 dbar Global max surface height on tracer cells (tau) = 1.00144525643314020E+00 m Global min surface height on tracer cells (tau) = -3.67609176291458351E+00 m Area average surface height on tracer cells (tau) = -4.71452865764730635E-03 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -1.70352893300665625E+12 m^3 Total Mass change = -2.37242062667895703E+12 kg Mass of ocean tracer cells (tau) = 1.33675397108793396E+21 kg Mass from sources = -1.83105468750000000E-04 kg Mass from eta smoothing = -1.83105468750000000E-04 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -5.39911694740966406E+12 kg Mass of river runoff liquid water input = 5.49195731757010460E+08 kg Mass of sea ice melt input = 3.02614712592181934E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = -9.22869132041931152E+02 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96652045533584426E+25 J Total heat change of full system for (taup1-taum1) = 6.74884510646307389E+19 J Total heat input to ocean referenced to 0degC = 6.74883897315602514E+19 J Heat input via surface heat fluxes = 6.76381186467299820E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -2.35366683202278656E+17 J Heat input via river runoff = 3.61233497939395781E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 8.56016446827523040E+16 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = -1.37820357812500000E+06 J Heat input via eta_t smooth = 8.00000000000000000E+00 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 6.74884510646307389E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 6.13330718657555781E+13 J Mismatch converted to a surface flux = 4.71499223644429805E-05 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161572632339907E+19 kg Total tracer change in system for (taup1-taum1) = 1.21045785705872803E+10 kg Total tracer input to ocean = 1.21045785733302650E+10 kg Tracer input via surface fluxes = 1.21045785733302612E+10 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = -1.13090863227844238E+01 kg Tracer input via eta_t smoother = 4.29153442382812500E-06 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 1.21634915544903278E+10 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = 8.60779276730489684E+00 kg Mismatch converted to a surface flux = 6.61725800390317352E-18 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 1.01933036591015214E-01 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066581565019136E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758092456714299E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758092456714354E-04 yr Age input via sources in th_tendency, or errors = 1.78282853896444363E-20 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.11668398703812074E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -2.08969375290222463E-06 yr Mismatch converted to a surface flux = -5.06959045701975920E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 935 idate: 10209 sec: 0 MATM istep1: 959 idate: 10210 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/10 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/10 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347841604561E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5832.2298 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347841604072E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.465015801020E+05 The minimum dzt is 4.774301061165E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 39.7485 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.774301060091E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.940950119096E+03 The minimum T is -2.074397350315E+00 deg C at (i,j,k) = ( 241, 2, 29), (lon,lat,dpt) = ( -39.5000, -77.6297, 812.7816 m) yyyy/mm/dd hh:mm:ss = 1/ 2/10 0: 0: 0 Tracer integrals for temp The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 5.025638973031E+01 m) The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.201528584472E+04 And the number of cells in the column are kmt = 29 The maximum T is 3.056001598369E+01 deg C at (i,j,k) = ( 60, 92, 1), (lon,lat,dpt) = ( -220.5000, -17.1490, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.062513287499E+05, 7.606978203305E+04, 1.016314994248E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.051824011131E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68519160907866539E+00 Variance temp = 2.01780692505983268E+01 |dT/dt| temp = 1.52897177694991537E+00 Total temp = 1.96658753106447436E+25 yyyy/mm/dd hh:mm:ss = 1/ 2/10 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/10 0: 0: 0 Tracer integrals for salt The maximum S is 4.058526181675E+01 psu at (i,j,k) = ( 332, 195, 4), (lon,lat,dpt) = ( 51.5000, 27.5082, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 1.001017001513E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.035979341513E+04 And the number of cells in the column are kmt = 5 The minimum S is 6.334994638046E+00 psu at (i,j,k) = ( 304, 235, 1), (lon,lat,dpt) = ( 23.5000, 59.9708, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.564647372818E+04, 5.780019800035E+04, 9.866492578768E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021585843389E+04 And the number of cells in the column are kmt = 5 Average salt = 3.47230401955471208E+01 Variance salt = 1.46091020238827696E-01 |dT/dt| salt = 1.76435555856990056E-01 Total salt = 4.64161578528133939E+19 yyyy/mm/dd hh:mm:ss = 1/ 2/10 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/10 0: 0: 0 Tracer integrals for age_global The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.869219386019E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021472959631E+04 And the number of cells in the column are kmt = 12 The maximum age_global is 1.093999543953E-01 yr at (i,j,k) = ( 338, 281, 5), (lon,lat,dpt) = ( 65.6026, 71.5268, 45.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.693914597147E+04, 2.592186576923E+04, 9.846002478247E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.019046516101E+04 And the number of cells in the column are kmt = 9 Average age_global = 1.07277156158614981E-01 Variance age_global = 2.01813417332599374E-04 |dT/dt| age_global = 9.15380481755806441E-02 Total age_global = 1.43403152092014723E+20 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 2/10 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.67727474051490444E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -2.31778567703161409E+00 dbar Global max surface height on tracer cells (tau) = 9.97021198919825768E-01 m Global min surface height on tracer cells (tau) = -3.67460528166913480E+00 m Area average surface height on tracer cells (tau) = -5.02385303292136355E-03 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -1.81529896586218384E+12 m^3 Total Mass change = -2.45947340811549023E+12 kg Mass of ocean tracer cells (tau) = 1.33675385540594998E+21 kg Mass from sources = -1.37329101562500000E-04 kg Mass from eta smoothing = -1.37329101562500000E-04 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -5.56539639257112109E+12 kg Mass of river runoff liquid water input = 5.56303368778005838E+08 kg Mass of sea ice melt input = 3.10536668142352002E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = -3.36666540384292603E+02 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96658753106447436E+25 J Total heat change of full system for (taup1-taum1) = 6.09316491582737121E+19 J Total heat input to ocean referenced to 0degC = 6.09315995463182254E+19 J Heat input via surface heat fluxes = 6.11104642271051940E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -2.48143283684292256E+17 J Heat input via river runoff = 3.59487055618085156E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 6.92426541917598880E+16 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = 7.11099484375000000E+05 J Heat input via eta_t smooth = 2.00000000000000000E+01 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 6.09316491582737121E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 4.96119547756205156E+13 J Mismatch converted to a surface flux = 3.81392900251066887E-05 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161578528133939E+19 kg Total tracer change in system for (taup1-taum1) = 1.24214568478681641E+10 kg Total tracer input to ocean = 1.24214568241880207E+10 kg Tracer input via surface fluxes = 1.24214568241880188E+10 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = -7.06452608108520508E-01 kg Tracer input via eta_t smoother = 1.19209289550781250E-06 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 1.24819120783467369E+10 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = 2.45052855269906509E+01 kg Mismatch converted to a surface flux = 1.88384875397253707E-17 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 1.07277156158614981E-01 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066571265954464E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758094604155351E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758094604155338E-04 yr Age input via sources in th_tendency, or errors = 1.30738822719516469E-20 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.11455297891000695E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -2.30279671315466741E-06 yr Mismatch converted to a surface flux = -5.58657756680942682E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 983 idate: 10211 sec: 0 MATM istep1: 1007 idate: 10212 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/12 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/12 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347834898714E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5832.2181 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347834898226E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.465009248272E+05 The minimum dzt is 4.766943505857E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 39.6873 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.766943504785E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.934308032074E+03 The minimum T is -2.071912503761E+00 deg C at (i,j,k) = ( 241, 2, 29), (lon,lat,dpt) = ( -39.5000, -77.6297, 812.7816 m) yyyy/mm/dd hh:mm:ss = 1/ 2/12 0: 0: 0 Tracer integrals for temp The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 5.025766776026E+01 m) The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.201681070484E+04 And the number of cells in the column are kmt = 29 The maximum T is 3.060444184992E+01 deg C at (i,j,k) = ( 60, 92, 2), (lon,lat,dpt) = ( -220.5000, -17.1490, 15.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.062513287499E+05, 7.606978203305E+04, 1.016457151397E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.052073501872E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68529651874837327E+00 Variance temp = 2.01812655945929649E+01 |dT/dt| temp = 1.54117102193943034E+00 Total temp = 1.96664333986845644E+25 yyyy/mm/dd hh:mm:ss = 1/ 2/12 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/12 0: 0: 0 Tracer integrals for salt The maximum S is 4.058963845042E+01 psu at (i,j,k) = ( 332, 195, 3), (lon,lat,dpt) = ( 51.5000, 27.5082, 25.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 1.000394285511E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.035443445281E+04 And the number of cells in the column are kmt = 5 The minimum S is 6.329746007908E+00 psu at (i,j,k) = ( 304, 235, 1), (lon,lat,dpt) = ( 23.5000, 59.9708, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.564647372818E+04, 5.780019800035E+04, 9.846375648453E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.019099916373E+04 And the number of cells in the column are kmt = 5 Average salt = 3.47230437519377091E+01 Variance salt = 1.46066801246661271E-01 |dT/dt| salt = 1.73887364559819152E-01 Total salt = 4.64161584572949791E+19 yyyy/mm/dd hh:mm:ss = 1/ 2/12 0: 0: 0 The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.865933245621E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021121994460E+04 yyyy/mm/dd hh:mm:ss = 1/ 2/12 0: 0: 0 Tracer integrals for age_global And the number of cells in the column are kmt = 12 The maximum age_global is 1.148756559709E-01 yr at (i,j,k) = ( 338, 281, 5), (lon,lat,dpt) = ( 65.6026, 71.5268, 45.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.693914597147E+04, 2.592186576923E+04, 9.833383076960E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.017779525267E+04 And the number of cells in the column are kmt = 9 Average age_global = 1.12616784112698515E-01 Variance age_global = 2.25811752684537334E-04 |dT/dt| age_global = 9.16166848209570284E-02 Total age_global = 1.50540906887930577E+20 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 2/12 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.69244327575080100E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -2.33116115822037706E+00 dbar Global max surface height on tracer cells (tau) = 9.99669574625711599E-01 m Global min surface height on tracer cells (tau) = -3.65631915150384801E+00 m Area average surface height on tracer cells (tau) = -5.34339675773783281E-03 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -1.93076161761690259E+12 m^3 Total Mass change = -2.52120324219463867E+12 kg Mass of ocean tracer cells (tau) = 1.33675373590210517E+21 kg Mass from sources = 7.62939453125000000E-06 kg Mass from eta smoothing = 7.62939453125000000E-06 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -5.69832458789647461E+12 kg Mass of river runoff liquid water input = 5.60181441947713137E+08 kg Mass of sea ice melt input = 3.17656116472342188E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = -4.63533658266067505E+02 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96664333986845644E+25 J Total heat change of full system for (taup1-taum1) = 6.49073817434371195E+19 J Total heat input to ocean referenced to 0degC = 6.49073404636560589E+19 J Heat input via surface heat fluxes = 6.50319893330552914E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -1.82298856261255872E+17 J Heat input via river runoff = 3.64099028603857969E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 5.76135769591655840E+16 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = 1.58330203125000000E+05 J Heat input via eta_t smooth = -2.80000000000000000E+01 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 6.49073817434371195E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 4.12797809022777969E+13 J Mismatch converted to a surface flux = 3.17339146003271300E-05 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161584572949791E+19 kg Total tracer change in system for (taup1-taum1) = 1.27062347374062500E+10 kg Total tracer input to ocean = 1.27062347247456074E+10 kg Tracer input via surface fluxes = 1.27062347247456131E+10 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = 3.12780857086181641E-01 kg Tracer input via eta_t smoother = -6.19888305664062500E-06 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 1.27680759818732052E+10 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = 1.24079588100342750E+01 kg Mismatch converted to a surface flux = 9.53864329304803050E-18 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 1.12616784112698515E-01 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066560423297792E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758096668032334E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758096668032334E-04 yr Age input via sources in th_tendency, or errors = 1.51632501513457789E-20 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.11513074103745046E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -2.24502256428728288E-06 yr Mismatch converted to a surface flux = -5.44641766378356261E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 1031 idate: 10213 sec: 0 MATM istep1: 1055 idate: 10214 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/14 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/14 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347836769488E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5832.2214 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347836768999E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.465011468384E+05 The minimum dzt is 4.755348116573E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 39.5907 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.755348115503E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.922030297197E+03 The minimum T is -2.069419381999E+00 deg C at (i,j,k) = ( 241, 2, 29), (lon,lat,dpt) = ( -39.5000, -77.6297, 812.7816 m) yyyy/mm/dd hh:mm:ss = 1/ 2/14 0: 0: 0 Tracer integrals for temp The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 5.025596663456E+01 m) The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.201489527097E+04 And the number of cells in the column are kmt = 29 The maximum T is 3.064841976323E+01 deg C at (i,j,k) = ( 60, 92, 4), (lon,lat,dpt) = ( -220.5000, -17.1490, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.062513287499E+05, 7.606978203305E+04, 1.016314937012E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.051775473676E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68539216264679714E+00 Variance temp = 2.01841118495094989E+01 |dT/dt| temp = 1.52407173928341821E+00 Total temp = 1.96669420529825788E+25 yyyy/mm/dd hh:mm:ss = 1/ 2/14 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/14 0: 0: 0 Tracer integrals for salt The maximum S is 4.058794751089E+01 psu at (i,j,k) = ( 332, 195, 3), (lon,lat,dpt) = ( 51.5000, 27.5082, 25.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 1.002374300055E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.037545677410E+04 And the number of cells in the column are kmt = 5 The minimum S is 6.324089444763E+00 psu at (i,j,k) = ( 304, 235, 1), (lon,lat,dpt) = ( 23.5000, 59.9708, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.564647372818E+04, 5.780019800035E+04, 9.903957273890E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.025004017329E+04 And the number of cells in the column are kmt = 5 Average salt = 3.47230472827887979E+01 Variance salt = 1.46048913435606664E-01 |dT/dt| salt = 1.72169297425941420E-01 Total salt = 4.64161590577542595E+19 yyyy/mm/dd hh:mm:ss = 1/ 2/14 0: 0: 0 The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.866093659951E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021148353499E+04 yyyy/mm/dd hh:mm:ss = 1/ 2/14 0: 0: 0 Tracer integrals for age_global And the number of cells in the column are kmt = 12 The maximum age_global is 1.203513575464E-01 yr at (i,j,k) = ( 338, 281, 5), (lon,lat,dpt) = ( 65.6026, 71.5268, 45.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.693914597147E+04, 2.592186576923E+04, 9.815309137220E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.015868683671E+04 And the number of cells in the column are kmt = 9 Average age_global = 1.17958292816299257E-01 Variance age_global = 2.50714160039341993E-04 |dT/dt| age_global = 9.24943449717425814E-02 Total age_global = 1.57681174608669213E+20 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 2/14 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.69014813192300517E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -2.34431842275010416E+00 dbar Global max surface height on tracer cells (tau) = 9.99947781645889378E-01 m Global min surface height on tracer cells (tau) = -3.68865156467063926E+00 m Area average surface height on tracer cells (tau) = -5.66062114345688636E-03 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -2.04538620865658179E+12 m^3 Total Mass change = -2.48038622829374219E+12 kg Mass of ocean tracer cells (tau) = 1.33675361726565371E+21 kg Mass from sources = -6.10351562500000000E-05 kg Mass from eta smoothing = -6.10351562500000000E-05 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -5.61786423174870508E+12 kg Mass of river runoff liquid water input = 5.43657497585830927E+08 kg Mass of sea ice melt input = 3.13693434501768213E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = 9.39695480108261108E+02 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96669420529825788E+25 J Total heat change of full system for (taup1-taum1) = 5.36426362093629522E+19 J Total heat input to ocean referenced to 0degC = 5.36425929183277875E+19 J Heat input via surface heat fluxes = 5.38456105073866916E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -2.63473792855109120E+17 J Heat input via river runoff = 3.55663128591634219E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 6.04206374833436800E+16 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = 1.10178057812500000E+06 J Heat input via eta_t smooth = 1.60000000000000000E+01 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 5.36426362093629522E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 4.32910340628914219E+13 J Mismatch converted to a surface flux = 3.32800695130589712E-05 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161590577542595E+19 kg Total tracer change in system for (taup1-taum1) = 1.25477273376245728E+10 kg Total tracer input to ocean = 1.25477273302306786E+10 kg Tracer input via surface fluxes = 1.25477273302306824E+10 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = -5.30236506462097168E+00 kg Tracer input via eta_t smoother = -3.09944152832031250E-06 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 1.26087971265767918E+10 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = 1.27580519539968957E+01 kg Mismatch converted to a surface flux = 9.80777810165978944E-18 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 1.17958292816299257E-01 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066548360863904E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758097736875373E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758097736875373E-04 yr Age input via sources in th_tendency, or errors = 1.14316129995689141E-20 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.11380294019948546E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -2.37780371692682330E-06 yr Mismatch converted to a surface flux = -5.76854432150965940E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 1079 idate: 10215 sec: 0 MATM istep1: 1103 idate: 10216 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/16 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/16 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347837258270E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5832.2222 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347837257782E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.465011437928E+05 The minimum dzt is 4.756292035711E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 39.5986 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.756292034641E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.922768230408E+03 The minimum T is -2.066936734745E+00 deg C at (i,j,k) = ( 241, 2, 29), (lon,lat,dpt) = ( -39.5000, -77.6297, 812.7816 m) yyyy/mm/dd hh:mm:ss = 1/ 2/16 0: 0: 0 Tracer integrals for temp The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 5.025507149238E+01 m) The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.201401015704E+04 And the number of cells in the column are kmt = 29 The maximum T is 3.062290460784E+01 deg C at (i,j,k) = ( 60, 92, 1), (lon,lat,dpt) = ( -220.5000, -17.1490, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.062513287499E+05, 7.606978203305E+04, 1.016176057619E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.051882184062E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68542232264333824E+00 Variance temp = 2.01852986783880759E+01 |dT/dt| temp = 1.55616935296827785E+00 Total temp = 1.96671012372028789E+25 yyyy/mm/dd hh:mm:ss = 1/ 2/16 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/16 0: 0: 0 Tracer integrals for salt The maximum S is 4.058310282816E+01 psu at (i,j,k) = ( 332, 195, 1), (lon,lat,dpt) = ( 51.5000, 27.5082, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 1.002137945840E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.037202999614E+04 And the number of cells in the column are kmt = 5 The minimum S is 6.318469151343E+00 psu at (i,j,k) = ( 304, 235, 1), (lon,lat,dpt) = ( 23.5000, 59.9708, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.564647372818E+04, 5.780019800035E+04, 9.884923419618E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.022458750485E+04 And the number of cells in the column are kmt = 5 Average salt = 3.47230508531315749E+01 Variance salt = 1.46033938916616535E-01 |dT/dt| salt = 1.70532141358824441E-01 Total salt = 4.64161596687617556E+19 yyyy/mm/dd hh:mm:ss = 1/ 2/16 0: 0: 0 The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.864844911632E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.020999694190E+04 yyyy/mm/dd hh:mm:ss = 1/ 2/16 0: 0: 0 Tracer integrals for age_global And the number of cells in the column are kmt = 12 The maximum age_global is 1.258270591220E-01 yr at (i,j,k) = ( 338, 282, 7), (lon,lat,dpt) = ( 66.1728, 71.6756, 65.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.674370376030E+04, 2.604023624077E+04, 9.810488525477E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.016238788103E+04 And the number of cells in the column are kmt = 8 Average age_global = 1.23290413536698534E-01 Variance age_global = 2.78276984801159935E-04 |dT/dt| age_global = 9.35186236841654694E-02 Total age_global = 1.64808891492636656E+20 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 2/16 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.70492347042150794E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -2.35660584476776425E+00 dbar Global max surface height on tracer cells (tau) = 1.00945802306511045E+00 m Global min surface height on tracer cells (tau) = -3.70357288747616265E+00 m Area average surface height on tracer cells (tau) = -5.98109842719006697E-03 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -2.16118618885721094E+12 m^3 Total Mass change = -2.46926360269587500E+12 kg Mass of ocean tracer cells (tau) = 1.33675349741267399E+21 kg Mass from sources = -1.14440917968750000E-04 kg Mass from eta smoothing = -1.14440917968750000E-04 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -5.59177636205329980E+12 kg Mass of river runoff liquid water input = 5.31637440866375268E+08 kg Mass of sea ice melt input = 3.12198112251628613E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = -5.99727588951587677E+02 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96671012372028789E+25 J Total heat change of full system for (taup1-taum1) = 5.75868159297084539E+19 J Total heat input to ocean referenced to 0degC = 5.75867745107284378E+19 J Heat input via surface heat fluxes = 5.77272969751740498E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -1.98365764314877760E+17 J Heat input via river runoff = 3.54635526200182656E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 5.78078363166353600E+16 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = 4.75784573437500000E+06 J Heat input via eta_t smooth = -8.00000000000000000E+00 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 5.75868159297084539E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 4.14189752582822656E+13 J Mismatch converted to a surface flux = 3.18409205414863200E-05 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161596687617556E+19 kg Total tracer change in system for (taup1-taum1) = 1.24879144428137207E+10 kg Total tracer input to ocean = 1.24879144412956982E+10 kg Tracer input via surface fluxes = 1.24879144412957001E+10 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = -2.09814202785491943E+00 kg Tracer input via eta_t smoother = -2.50339508056640625E-06 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 1.25486931224068947E+10 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = 3.63376443802463989E+00 kg Mismatch converted to a surface flux = 2.79346372082165500E-18 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 1.23290413536698534E-01 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066540459197152E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758102024363625E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758102024363625E-04 yr Age input via sources in th_tendency, or errors = -7.57198319532240532E-20 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.11236924106733671E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -2.52117791762994850E-06 yr Mismatch converted to a surface flux = -6.11636968044463803E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 1127 idate: 10217 sec: 0 MATM istep1: 1151 idate: 10218 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/18 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/18 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347828560241E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5832.2071 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347828559752E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.465002750856E+05 The minimum dzt is 4.766092293492E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 39.6802 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.766092292420E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.932494431093E+03 yyyy/mm/dd hh:mm:ss = 1/ 2/18 0: 0: 0 Tracer integrals for temp The minimum T is -2.064474950279E+00 deg C at (i,j,k) = ( 241, 2, 29), (lon,lat,dpt) = ( -39.5000, -77.6297, 812.7816 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 5.025595018483E+01 m) The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.201506235440E+04 And the number of cells in the column are kmt = 29 The maximum T is 3.056694106560E+01 deg C at (i,j,k) = ( 60, 92, 1), (lon,lat,dpt) = ( -220.5000, -17.1490, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.062513287499E+05, 7.606978203305E+04, 1.018114142832E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.053971595051E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68554515044639208E+00 Variance temp = 2.01892060781756300E+01 |dT/dt| temp = 1.56311959893975061E+00 Total temp = 1.96677550008905543E+25 yyyy/mm/dd hh:mm:ss = 1/ 2/18 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/18 0: 0: 0 Tracer integrals for salt The maximum S is 4.058368347453E+01 psu at (i,j,k) = ( 332, 195, 4), (lon,lat,dpt) = ( 51.5000, 27.5082, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 9.995172526124E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.034936018238E+04 And the number of cells in the column are kmt = 5 The minimum S is 6.313807557183E+00 psu at (i,j,k) = ( 304, 235, 1), (lon,lat,dpt) = ( 23.5000, 59.9708, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.564647372818E+04, 5.780019800035E+04, 9.875392515180E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.022332099927E+04 And the number of cells in the column are kmt = 5 Average salt = 3.47230542980959669E+01 Variance salt = 1.46017084658069507E-01 |dT/dt| salt = 1.71040204405425417E-01 Total salt = 4.64161602577533829E+19 yyyy/mm/dd hh:mm:ss = 1/ 2/18 0: 0: 0 The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.866378352924E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021181850042E+04 yyyy/mm/dd hh:mm:ss = 1/ 2/18 0: 0: 0 Tracer integrals for age_global And the number of cells in the column are kmt = 12 The maximum age_global is 1.313027606976E-01 yr at (i,j,k) = ( 338, 282, 7), (lon,lat,dpt) = ( 66.1728, 71.6756, 65.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.674370376030E+04, 2.604023624077E+04, 9.825559871166E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.017638407875E+04 And the number of cells in the column are kmt = 8 Average age_global = 1.28626908097859510E-01 Variance age_global = 3.06354320812697589E-04 |dT/dt| age_global = 9.45565997469784147E-02 Total age_global = 1.71942454384174006E+20 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 2/18 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.70920132441371697E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -2.34774660839857541E+00 dbar Global max surface height on tracer cells (tau) = 1.00849588624862041E+00 m Global min surface height on tracer cells (tau) = -3.68097351664434846E+00 m Area average surface height on tracer cells (tau) = -6.29036464548682946E-03 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -2.27293520750311719E+12 m^3 Total Mass change = -2.35915957553394141E+12 kg Mass of ocean tracer cells (tau) = 1.33675338175243983E+21 kg Mass from sources = 1.14440917968750000E-05 kg Mass from eta smoothing = 1.14440917968750000E-05 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -5.37081517063445117E+12 kg Mass of river runoff liquid water input = 5.21817200510892153E+08 kg Mass of sea ice melt input = 3.01113377729878809E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = 6.01210776090621948E+02 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96677550008905543E+25 J Total heat change of full system for (taup1-taum1) = 5.81343868248688722E+19 J Total heat input to ocean referenced to 0degC = 5.81343394294436495E+19 J Heat input via surface heat fluxes = 5.82342151119000535E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -1.66059746445667712E+17 J Heat input via river runoff = 3.49960854774790312E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 6.61490679037812800E+16 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = -2.69055031250000000E+05 J Heat input via eta_t smooth = 2.40000000000000000E+01 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 5.81343868248688722E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 4.73954254917110312E+13 J Mismatch converted to a surface flux = 3.64353286796910547E-05 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161602577533829E+19 kg Total tracer change in system for (taup1-taum1) = 1.20445250110510254E+10 kg Total tracer input to ocean = 1.20445250049203434E+10 kg Tracer input via surface fluxes = 1.20445250049203339E+10 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = -9.48572659492492676E+00 kg Tracer input via eta_t smoother = 8.82148742675781250E-06 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 1.21031457142798100E+10 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = 1.56924136470925806E+01 kg Mismatch converted to a surface flux = 1.20635745555123703E-17 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 1.28626908097859510E-01 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066525685453632E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758100805754387E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758100805754387E-04 yr Age input via sources in th_tendency, or errors = 1.88773601690487330E-20 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.11377721937004333E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -2.38037886875005075E-06 yr Mismatch converted to a surface flux = -5.77479163171493757E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 1175 idate: 10219 sec: 0 MATM istep1: 1199 idate: 10220 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/20 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/20 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347832819658E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5832.2145 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347832819170E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.465006444879E+05 The minimum dzt is 4.776368898635E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 39.7657 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.776368897560E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.942939450676E+03 yyyy/mm/dd hh:mm:ss = 1/ 2/20 0: 0: 0 Tracer integrals for temp The minimum T is -2.062027999549E+00 deg C at (i,j,k) = ( 241, 2, 29), (lon,lat,dpt) = ( -39.5000, -77.6297, 812.7816 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 5.025738795774E+01 m) The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.201648290671E+04 And the number of cells in the column are kmt = 29 The maximum T is 3.061090690923E+01 deg C at (i,j,k) = ( 60, 92, 2), (lon,lat,dpt) = ( -220.5000, -17.1490, 15.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.062513287499E+05, 7.606978203305E+04, 1.017479159190E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.053126902912E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68559320932634638E+00 Variance temp = 2.01905494365772711E+01 |dT/dt| temp = 1.56674888531123169E+00 Total temp = 1.96680098094229449E+25 yyyy/mm/dd hh:mm:ss = 1/ 2/20 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/20 0: 0: 0 Tracer integrals for salt The maximum S is 4.058907970920E+01 psu at (i,j,k) = ( 332, 195, 5), (lon,lat,dpt) = ( 51.5000, 27.5082, 45.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 9.938684304168E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.028581815134E+04 And the number of cells in the column are kmt = 5 The minimum S is 6.309652647202E+00 psu at (i,j,k) = ( 304, 235, 1), (lon,lat,dpt) = ( 23.5000, 59.9708, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.564647372818E+04, 5.780019800035E+04, 9.875971329161E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.022123511463E+04 And the number of cells in the column are kmt = 5 Average salt = 3.47230576502989194E+01 Variance salt = 1.46001566371069202E-01 |dT/dt| salt = 1.70112988186918251E-01 Total salt = 4.64161608315469824E+19 yyyy/mm/dd hh:mm:ss = 1/ 2/20 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/20 0: 0: 0 Tracer integrals for age_global The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.868683064591E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021432314976E+04 And the number of cells in the column are kmt = 12 The maximum age_global is 1.367784622732E-01 yr at (i,j,k) = ( 338, 281, 7), (lon,lat,dpt) = ( 65.6026, 71.5268, 65.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.693914597147E+04, 2.592186576923E+04, 9.834615035869E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.017958460952E+04 And the number of cells in the column are kmt = 9 Average age_global = 1.33960939053326511E-01 Variance age_global = 3.36082714891435680E-04 |dT/dt| age_global = 9.52166721900803426E-02 Total age_global = 1.79072723228069134E+20 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 2/20 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.70400088304169484E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -2.30183989523770283E+00 dbar Global max surface height on tracer cells (tau) = 1.00483292607855001E+00 m Global min surface height on tracer cells (tau) = -3.63689862439771394E+00 m Area average surface height on tracer cells (tau) = -6.59125234651789047E-03 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -2.38165676622369922E+12 m^3 Total Mass change = -2.35069077192833789E+12 kg Mass of ocean tracer cells (tau) = 1.33675326922562653E+21 kg Mass from sources = 4.57763671875000000E-05 kg Mass from eta smoothing = 4.57763671875000000E-05 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -5.33554890102477539E+12 kg Mass of river runoff liquid water input = 5.19149339007850587E+08 kg Mass of sea ice melt input = 2.98433898009606299E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = -3.38632896363735199E+02 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96680098094229449E+25 J Total heat change of full system for (taup1-taum1) = 5.03347951883813192E+19 J Total heat input to ocean referenced to 0degC = 5.03347448319542559E+19 J Heat input via surface heat fluxes = 5.04335193680752312E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -1.69091600173278976E+17 J Heat input via river runoff = 3.53666472233899687E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 7.02816974050780640E+16 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = 6.92858031250000000E+05 J Heat input via eta_t smooth = 4.00000000000000000E+01 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 5.03347951883813192E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 5.03564263704379687E+13 J Mismatch converted to a surface flux = 3.87116040610807196E-05 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161608315469824E+19 kg Total tracer change in system for (taup1-taum1) = 1.19373456240846405E+10 kg Total tracer input to ocean = 1.19373456145347824E+10 kg Tracer input via surface fluxes = 1.19373456145347900E+10 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = 2.17639935016632080E+00 kg Tracer input via eta_t smoother = -7.74860382080078125E-06 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 1.19954446852370605E+10 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = 7.40934536679804268E+00 kg Mismatch converted to a surface flux = 5.69594915416143509E-18 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 1.33960939053326511E-01 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066518359557408E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758104900733706E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758104900733706E-04 yr Age input via sources in th_tendency, or errors = -1.26326369783092454E-20 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.11310025427389743E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -2.44807947334396386E-06 yr Mismatch converted to a surface flux = -5.93903308504134211E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 1223 idate: 10221 sec: 0 MATM istep1: 1247 idate: 10222 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/22 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/22 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347831257221E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5832.2118 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347831256732E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.465005544990E+05 The minimum dzt is 4.770194890932E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 39.7143 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.770194889859E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.936936466784E+03 yyyy/mm/dd hh:mm:ss = 1/ 2/22 0: 0: 0 Tracer integrals for temp The minimum T is -2.059597456193E+00 deg C at (i,j,k) = ( 241, 2, 29), (lon,lat,dpt) = ( -39.5000, -77.6297, 812.7816 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 5.025578693162E+01 m) The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.201485492610E+04 And the number of cells in the column are kmt = 29 The maximum T is 3.067298242920E+01 deg C at (i,j,k) = ( 60, 92, 4), (lon,lat,dpt) = ( -220.5000, -17.1490, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.062513287499E+05, 7.606978203305E+04, 1.015971043359E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.051458426187E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68564977669716631E+00 Variance temp = 2.01933230833743842E+01 |dT/dt| temp = 1.52733832828319627E+00 Total temp = 1.96683099901615461E+25 yyyy/mm/dd hh:mm:ss = 1/ 2/22 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/22 0: 0: 0 Tracer integrals for salt The maximum S is 4.058443819569E+01 psu at (i,j,k) = ( 332, 195, 2), (lon,lat,dpt) = ( 51.5000, 27.5082, 15.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 1.004818266573E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.039902249680E+04 And the number of cells in the column are kmt = 5 The minimum S is 6.306351343449E+00 psu at (i,j,k) = ( 304, 235, 1), (lon,lat,dpt) = ( 23.5000, 59.9708, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.564647372818E+04, 5.780019800035E+04, 9.912907847706E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.026076693491E+04 And the number of cells in the column are kmt = 5 Average salt = 3.47230610717623662E+01 Variance salt = 1.45971206907915985E-01 |dT/dt| salt = 1.64913638248001926E-01 Total salt = 4.64161614201809633E+19 yyyy/mm/dd hh:mm:ss = 1/ 2/22 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/22 0: 0: 0 Tracer integrals for age_global The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.867336309275E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021260864516E+04 And the number of cells in the column are kmt = 12 The maximum age_global is 1.422541638487E-01 yr at (i,j,k) = ( 338, 281, 7), (lon,lat,dpt) = ( 65.6026, 71.5268, 65.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.693914597147E+04, 2.592186576923E+04, 9.830853699453E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.017514704139E+04 And the number of cells in the column are kmt = 9 Average age_global = 1.39293064815236706E-01 Variance age_global = 3.67167777355417724E-04 |dT/dt| age_global = 9.64055797239830314E-02 Total age_global = 1.86200443786150412E+20 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 2/22 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.70112290475852790E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -2.29779321677079418E+00 dbar Global max surface height on tracer cells (tau) = 1.00020983793815099E+00 m Global min surface height on tracer cells (tau) = -3.65963967527224243E+00 m Area average surface height on tracer cells (tau) = -6.89812681001927656E-03 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -2.49254155775583594E+12 m^3 Total Mass change = -2.41495079576181250E+12 kg Mass of ocean tracer cells (tau) = 1.33675315445986728E+21 kg Mass from sources = -9.15527343750000000E-05 kg Mass from eta smoothing = -9.15527343750000000E-05 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -5.53506999945383496E+12 kg Mass of river runoff liquid water input = 5.00147646035899043E+08 kg Mass of sea ice melt input = 3.11961905603735254E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = 8.63411438465118408E+00 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96683099901615461E+25 J Total heat change of full system for (taup1-taum1) = 5.65920526576316416E+19 J Total heat input to ocean referenced to 0degC = 5.65920025829425725E+19 J Heat input via surface heat fluxes = 5.67270104048560046E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -2.04930403781204352E+17 J Heat input via river runoff = 3.40976357150586016E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 6.98884842320634560E+16 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = 1.06536939843750000E+06 J Heat input via eta_t smooth = -1.20000000000000000E+01 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 5.65920526576316416E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 5.00746880036866016E+13 J Mismatch converted to a surface flux = 3.84950171249414760E-05 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161614201809633E+19 kg Total tracer change in system for (taup1-taum1) = 1.24784658433349609E+10 kg Total tracer input to ocean = 1.24784658344756107E+10 kg Tracer input via surface fluxes = 1.24784658344756088E+10 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = 2.88451910018920898E+00 kg Tracer input via eta_t smoother = 2.38418579101562500E-06 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 1.25391985365944710E+10 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = 6.00391060726308812E+00 kg Mismatch converted to a surface flux = 4.61551835582469951E-18 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 1.39293064815236706E-01 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066504619462592E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758104394096101E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758104394096128E-04 yr Age input via sources in th_tendency, or errors = -2.13553825972506825E-20 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.11215664340568273E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -2.54244005352782088E-06 yr Mismatch converted to a surface flux = -6.16795155510642082E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 1271 idate: 10223 sec: 0 MATM istep1: 1295 idate: 10224 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/24 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/24 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347834494880E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5832.2174 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347834494391E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.465008515051E+05 The minimum dzt is 4.768299660655E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 39.6985 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.768299659582E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.934899185541E+03 The minimum T is -2.057183899169E+00 deg C at (i,j,k) = ( 241, 2, 29), (lon,lat,dpt) = ( -39.5000, -77.6297, 812.7816 m) yyyy/mm/dd hh:mm:ss = 1/ 2/24 0: 0: 0 Tracer integrals for temp The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 5.025487693551E+01 m) The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.201380582740E+04 And the number of cells in the column are kmt = 29 The maximum T is 3.072204943467E+01 deg C at (i,j,k) = ( 60, 92, 1), (lon,lat,dpt) = ( -220.5000, -17.1490, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.062513287499E+05, 7.606978203305E+04, 1.014168616876E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.049535868880E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68576962775466210E+00 Variance temp = 2.01989355868145068E+01 |dT/dt| temp = 1.56178036945096821E+00 Total temp = 1.96689478987441758E+25 yyyy/mm/dd hh:mm:ss = 1/ 2/24 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/24 0: 0: 0 Tracer integrals for salt The maximum S is 4.058924052227E+01 psu at (i,j,k) = ( 332, 195, 5), (lon,lat,dpt) = ( 51.5000, 27.5082, 45.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 9.949408080126E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.030113582303E+04 And the number of cells in the column are kmt = 5 The minimum S is 6.303579052199E+00 psu at (i,j,k) = ( 304, 235, 1), (lon,lat,dpt) = ( 23.5000, 59.9708, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.564647372818E+04, 5.780019800035E+04, 9.935754850686E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.028192068421E+04 And the number of cells in the column are kmt = 5 Average salt = 3.47230644625142659E+01 Variance salt = 1.45945389435610196E-01 |dT/dt| salt = 1.65361994555982772E-01 Total salt = 4.64161620085363507E+19 yyyy/mm/dd hh:mm:ss = 1/ 2/24 0: 0: 0 The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.868305660961E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021388894539E+04 yyyy/mm/dd hh:mm:ss = 1/ 2/24 0: 0: 0 Tracer integrals for age_global And the number of cells in the column are kmt = 12 The maximum age_global is 1.477298654243E-01 yr at (i,j,k) = ( 338, 281, 7), (lon,lat,dpt) = ( 65.6026, 71.5268, 65.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.693914597147E+04, 2.592186576923E+04, 9.828215674785E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.017297194032E+04 And the number of cells in the column are kmt = 9 Average age_global = 1.44626259113813993E-01 Variance age_global = 3.99188364461275369E-04 |dT/dt| age_global = 9.68322304792745836E-02 Total age_global = 1.93329591659815895E+20 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 2/24 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.71861876502223332E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -2.32210055851424135E+00 dbar Global max surface height on tracer cells (tau) = 1.08200249577256757E+00 m Global min surface height on tracer cells (tau) = -3.69655604108432279E+00 m Area average surface height on tracer cells (tau) = -7.20186123895172250E-03 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -2.60229174175299609E+12 m^3 Total Mass change = -2.31736496021526172E+12 kg Mass of ocean tracer cells (tau) = 1.33675304086842691E+21 kg Mass from sources = -1.22070312500000000E-04 kg Mass from eta smoothing = -1.22070312500000000E-04 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -5.29523230932871680E+12 kg Mass of river runoff liquid water input = 4.99252987580438137E+08 kg Mass of sea ice melt input = 2.97736809608319580E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = 4.26794495582580566E+01 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96689478987441758E+25 J Total heat change of full system for (taup1-taum1) = 6.36215218865042555E+19 J Total heat input to ocean referenced to 0degC = 6.36214663116759368E+19 J Heat input via surface heat fluxes = 6.37088784692637614E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -1.65011352911204224E+17 J Heat input via river runoff = 3.42608126062811836E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 7.75649345107749120E+16 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = -1.25901183593750000E+05 J Heat input via eta_t smooth = 4.00000000000000000E+00 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 6.36215218865042555E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 5.55748284446211875E+13 J Mismatch converted to a surface flux = 4.27232611520989193E-05 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161620085363507E+19 kg Total tracer change in system for (taup1-taum1) = 1.19094618719642334E+10 kg Total tracer input to ocean = 1.19094618801459312E+10 kg Tracer input via surface fluxes = 1.19094618801459274E+10 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = -1.37398102283477783E+01 kg Tracer input via eta_t smoother = 3.09944152832031250E-06 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 1.19674252228950825E+10 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = 5.58516371585631344E+00 kg Mismatch converted to a surface flux = 4.29360584077252252E-18 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 1.44626259113813993E-01 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066486023435712E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758100141118153E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758100141118140E-04 yr Age input via sources in th_tendency, or errors = 1.21241776024441876E-20 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.11325883172552312E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -2.43221696856585222E-06 yr Mismatch converted to a surface flux = -5.90055069845437810E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 1319 idate: 10225 sec: 0 MATM istep1: 1343 idate: 10226 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/26 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/26 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347835673362E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5832.2195 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347835672873E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.465009777401E+05 The minimum dzt is 4.764586548129E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 39.6676 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.764586547057E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.930904922218E+03 yyyy/mm/dd hh:mm:ss = 1/ 2/26 0: 0: 0 Tracer integrals for temp The minimum T is -2.054796702593E+00 deg C at (i,j,k) = ( 241, 2, 29), (lon,lat,dpt) = ( -39.5000, -77.6297, 812.7816 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 5.025513243604E+01 m) The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.201398518385E+04 And the number of cells in the column are kmt = 29 The maximum T is 3.077340131602E+01 deg C at (i,j,k) = ( 60, 92, 4), (lon,lat,dpt) = ( -220.5000, -17.1490, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.062513287499E+05, 7.606978203305E+04, 1.015106587065E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.050624818833E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68592637405595580E+00 Variance temp = 2.02055921994490433E+01 |dT/dt| temp = 1.49538506405320781E+00 Total temp = 1.96697826947639555E+25 yyyy/mm/dd hh:mm:ss = 1/ 2/26 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/26 0: 0: 0 Tracer integrals for salt The maximum S is 4.059423171590E+01 psu at (i,j,k) = ( 315, 195, 5), (lon,lat,dpt) = ( 34.5000, 27.5082, 45.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 1.001141600635E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.036236182588E+04 And the number of cells in the column are kmt = 5 The minimum S is 6.301413386418E+00 psu at (i,j,k) = ( 304, 235, 1), (lon,lat,dpt) = ( 23.5000, 59.9708, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.564647372818E+04, 5.780019800035E+04, 9.958543355630E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.031075091905E+04 And the number of cells in the column are kmt = 5 Average salt = 3.47230678596865303E+01 Variance salt = 1.45920207057315565E-01 |dT/dt| salt = 1.58679648315369071E-01 Total salt = 4.64161626000763945E+19 yyyy/mm/dd hh:mm:ss = 1/ 2/26 0: 0: 0 The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.867069888372E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021266964247E+04 yyyy/mm/dd hh:mm:ss = 1/ 2/26 0: 0: 0 Tracer integrals for age_global And the number of cells in the column are kmt = 12 The maximum age_global is 1.532055669999E-01 yr at (i,j,k) = ( 338, 281, 7), (lon,lat,dpt) = ( 65.6026, 71.5268, 65.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.693914597147E+04, 2.592186576923E+04, 9.831547252085E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.017564796202E+04 And the number of cells in the column are kmt = 9 Average age_global = 1.49965434792084934E-01 Variance age_global = 4.31201732022344630E-04 |dT/dt| age_global = 9.58264830143243096E-02 Total age_global = 2.00466733925376360E+20 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 2/26 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.71408259586058564E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -2.26953835365828116E+00 dbar Global max surface height on tracer cells (tau) = 1.01568188722326003E+00 m Global min surface height on tracer cells (tau) = -3.69745862515132506E+00 m Area average surface height on tracer cells (tau) = -7.50601127721529232E-03 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -2.71219210036395313E+12 m^3 Total Mass change = -2.36842514787018652E+12 kg Mass of ocean tracer cells (tau) = 1.33675292712155585E+21 kg Mass from sources = -1.44958496093750000E-04 kg Mass from eta smoothing = -1.44958496093750000E-04 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -5.43117357895213574E+12 kg Mass of river runoff liquid water input = 4.91773562876060605E+08 kg Mass of sea ice melt input = 3.06225665693925098E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = 5.79822326540946960E+02 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96697826947639555E+25 J Total heat change of full system for (taup1-taum1) = 6.71285930638669005E+19 J Total heat input to ocean referenced to 0degC = 6.71285406199798907E+19 J Heat input via surface heat fluxes = 6.73136417613828096E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -2.58330008150495424E+17 J Heat input via river runoff = 3.37328496539405469E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 7.31951338979265760E+16 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = 1.80741145312500000E+06 J Heat input via eta_t smooth = -4.00000000000000000E+01 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 6.71285930638669005E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 5.24438852023805469E+13 J Mismatch converted to a surface flux = 4.03163422369296441E-05 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161626000763945E+19 kg Total tracer change in system for (taup1-taum1) = 1.22490161824451904E+10 kg Total tracer input to ocean = 1.22490161534640350E+10 kg Tracer input via surface fluxes = 1.22490161534640350E+10 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = 7.34142971038818359E+00 kg Tracer input via eta_t smoother = 9.53674316406250000E-07 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 1.23086321442051506E+10 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = 2.17450462300291036E+01 kg Mismatch converted to a surface flux = 1.67165480281372357E-17 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 1.49965434792084934E-01 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066471762696704E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758099157164824E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758099157164851E-04 yr Age input via sources in th_tendency, or errors = -1.25654297731213273E-20 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.11383282406730109E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -2.37481675043470715E-06 yr Mismatch converted to a surface flux = -5.76129795021585668E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 1367 idate: 10227 sec: 0 MATM istep1: 1391 idate: 10228 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/28 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/28 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347836006992E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5832.2200 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347836006503E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.465010392387E+05 The minimum dzt is 4.768609165104E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 39.7011 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.768609164031E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.935853354105E+03 yyyy/mm/dd hh:mm:ss = 1/ 2/28 0: 0: 0 Tracer integrals for temp The minimum T is -2.052429552820E+00 deg C at (i,j,k) = ( 241, 2, 29), (lon,lat,dpt) = ( -39.5000, -77.6297, 812.7816 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 5.025590874847E+01 m) The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.201478208162E+04 And the number of cells in the column are kmt = 29 The maximum T is 3.083483000308E+01 deg C at (i,j,k) = ( 60, 92, 4), (lon,lat,dpt) = ( -220.5000, -17.1490, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.062513287499E+05, 7.606978203305E+04, 1.015644736012E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.051282231760E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68609647190009992E+00 Variance temp = 2.02132311947837380E+01 |dT/dt| temp = 1.48438210403116777E+00 Total temp = 1.96706887524240744E+25 yyyy/mm/dd hh:mm:ss = 1/ 2/28 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 2/28 0: 0: 0 Tracer integrals for salt The maximum S is 4.060824510060E+01 psu at (i,j,k) = ( 315, 195, 3), (lon,lat,dpt) = ( 34.5000, 27.5082, 25.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 9.956366721888E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.030562589004E+04 And the number of cells in the column are kmt = 5 The minimum S is 6.299140862949E+00 psu at (i,j,k) = ( 304, 235, 1), (lon,lat,dpt) = ( 23.5000, 59.9708, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.564647372818E+04, 5.780019800035E+04, 9.892396246446E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.023953507048E+04 And the number of cells in the column are kmt = 5 Average salt = 3.47230712250308784E+01 Variance salt = 1.45892008576993248E-01 |dT/dt| salt = 1.56188649287155978E-01 Total salt = 4.64161631770840023E+19 yyyy/mm/dd hh:mm:ss = 1/ 2/28 0: 0: 0 The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.865936418422E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021118402357E+04 yyyy/mm/dd hh:mm:ss = 1/ 2/28 0: 0: 0 Tracer integrals for age_global And the number of cells in the column are kmt = 12 The maximum age_global is 1.586812685755E-01 yr at (i,j,k) = ( 338, 281, 7), (lon,lat,dpt) = ( 65.6026, 71.5268, 65.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.693914597147E+04, 2.592186576923E+04, 9.821599301589E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.016549787722E+04 And the number of cells in the column are kmt = 9 Average age_global = 1.55305095687867656E-01 Variance age_global = 4.64126919407222699E-04 |dT/dt| age_global = 9.64231886391131443E-02 Total age_global = 2.07604523717481136E+20 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 2/28 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.71789964451231070E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -2.30019723477978255E+00 dbar Global max surface height on tracer cells (tau) = 1.00605438093723065E+00 m Global min surface height on tracer cells (tau) = -3.68367823359408986E+00 m Area average surface height on tracer cells (tau) = -7.80800400919091052E-03 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -2.82131294654731641E+12 m^3 Total Mass change = -2.36163174034963867E+12 kg Mass of ocean tracer cells (tau) = 1.33675281418148014E+21 kg Mass from sources = 2.89916992187500000E-04 kg Mass from eta smoothing = 2.89916992187500000E-04 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -5.37070403126726465E+12 kg Mass of river runoff liquid water input = 4.81596889929839253E+08 kg Mass of sea ice melt input = 3.00859069494359668E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = -9.15900832295417786E+02 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96706887524240744E+25 J Total heat change of full system for (taup1-taum1) = 6.32454427426972795E+19 J Total heat input to ocean referenced to 0degC = 6.32454039134006559E+19 J Heat input via surface heat fluxes = 6.34539261188001055E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -2.62748482160010496E+17 J Heat input via river runoff = 3.28254650539888398E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 5.41934512955075760E+16 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = 5.32943160156250000E+05 J Heat input via eta_t smooth = 1.20000000000000000E+01 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 6.32454427426972795E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 3.88292960906728437E+13 J Mismatch converted to a surface flux = 2.98500994724086736E-05 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161631770840023E+19 kg Total tracer change in system for (taup1-taum1) = 1.20343523097785034E+10 kg Total tracer input to ocean = 1.20343523023641891E+10 kg Tracer input via surface fluxes = 1.20343523023641891E+10 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = -5.43017482757568359E+00 kg Tracer input via eta_t smoother = -9.53674316406250000E-07 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 1.20929235024701958E+10 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = 1.29070032260332095E+01 kg Mismatch converted to a surface flux = 9.92228469164388752E-18 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 1.55305095687867656E-01 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066464070854208E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758103013699124E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758103013699165E-04 yr Age input via sources in th_tendency, or errors = -7.19005641133845138E-20 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.11437006155217162E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -2.32109685848196634E-06 yr Mismatch converted to a surface flux = -5.63097366168433533E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 1415 idate: 10301 sec: 0 MATM istep1: 1439 idate: 10302 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 3/ 2 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 3/ 2 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347833378088E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5832.2155 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347833377599E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.465008068626E+05 The minimum dzt is 4.762554226258E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 39.6507 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.762554225187E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.929125791816E+03 yyyy/mm/dd hh:mm:ss = 1/ 3/ 2 0: 0: 0 Tracer integrals for temp The minimum T is -2.050090741341E+00 deg C at (i,j,k) = ( 241, 2, 29), (lon,lat,dpt) = ( -39.5000, -77.6297, 812.7816 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 5.025971903109E+01 m) The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.201874702650E+04 And the number of cells in the column are kmt = 29 The maximum T is 3.089451003812E+01 deg C at (i,j,k) = ( 60, 92, 4), (lon,lat,dpt) = ( -220.5000, -17.1490, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.062513287499E+05, 7.606978203305E+04, 1.016265905741E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.051723506239E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68627667554378435E+00 Variance temp = 2.02213921258879452E+01 |dT/dt| temp = 1.47008529548843558E+00 Total temp = 1.96716487709676527E+25 yyyy/mm/dd hh:mm:ss = 1/ 3/ 2 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 3/ 2 0: 0: 0 Tracer integrals for salt The maximum S is 4.061693256059E+01 psu at (i,j,k) = ( 315, 195, 5), (lon,lat,dpt) = ( 34.5000, 27.5082, 45.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 9.969019652235E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.031566667905E+04 And the number of cells in the column are kmt = 5 The minimum S is 6.296838787890E+00 psu at (i,j,k) = ( 304, 235, 1), (lon,lat,dpt) = ( 23.5000, 59.9708, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.564647372818E+04, 5.780019800035E+04, 9.887472677132E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.023403100254E+04 And the number of cells in the column are kmt = 5 Average salt = 3.47230745268852061E+01 Variance salt = 1.45869324390787369E-01 |dT/dt| salt = 1.55457831719309769E-01 Total salt = 4.64161637444774298E+19 yyyy/mm/dd hh:mm:ss = 1/ 3/ 2 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 3/ 2 0: 0: 0 Tracer integrals for age_global The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.867973224919E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021364317581E+04 And the number of cells in the column are kmt = 12 The maximum age_global is 1.641569701510E-01 yr at (i,j,k) = ( 338, 281, 7), (lon,lat,dpt) = ( 65.6026, 71.5268, 65.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.693914597147E+04, 2.592186576923E+04, 9.816395344515E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.016021051106E+04 And the number of cells in the column are kmt = 9 Average age_global = 1.60644280529679939E-01 Variance age_global = 4.98382456704835747E-04 |dT/dt| age_global = 9.77043321018234712E-02 Total age_global = 2.14741676285203874E+20 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 3/ 2 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.71274402278326465E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -2.33892394709736129E+00 dbar Global max surface height on tracer cells (tau) = 1.01729130640789944E+00 m Global min surface height on tracer cells (tau) = -3.61035835145657824E+00 m Area average surface height on tracer cells (tau) = -8.10420142252180585E-03 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -2.92833973546553516E+12 m^3 Total Mass change = -2.28608161816365234E+12 kg Mass of ocean tracer cells (tau) = 1.33675270340875361E+21 kg Mass from sources = 3.05175781250000000E-05 kg Mass from eta smoothing = 3.05175781250000000E-05 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -5.18749170786035645E+12 kg Mass of river runoff liquid water input = 4.72653728116113186E+08 kg Mass of sea ice melt input = 2.90093743591018848E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = 5.83994812965393066E+01 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96716487709676527E+25 J Total heat change of full system for (taup1-taum1) = 6.76057695952857006E+19 J Total heat input to ocean referenced to 0degC = 6.76057189312856637E+19 J Heat input via surface heat fluxes = 6.76961849947052442E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -1.61208763339468992E+17 J Heat input via river runoff = 3.17319900442857148E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 7.07109679298489680E+16 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = -1.94913171484375000E+06 J Heat input via eta_t smooth = 1.40000000000000000E+01 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 6.76057695952857006E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 5.06640019859957187E+13 J Mismatch converted to a surface flux = 3.89480534342098839E-05 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161637444774298E+19 kg Total tracer change in system for (taup1-taum1) = 1.16037393016624146E+10 kg Total tracer input to ocean = 1.16037392769575539E+10 kg Tracer input via surface fluxes = 1.16037392769575653E+10 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = 1.80091571807861328E+00 kg Tracer input via eta_t smoother = -1.23977661132812500E-05 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 1.16602147008436050E+10 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = 2.30154184693422295E+01 kg Mismatch converted to a surface flux = 1.76931492423836170E-17 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 1.60644280529679939E-01 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066459144260896E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758108748572502E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758108748572516E-04 yr Age input via sources in th_tendency, or errors = 4.09399303656075697E-20 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.11455251903378401E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -2.30285684519408876E-06 yr Mismatch converted to a surface flux = -5.58672344694750432E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 1463 idate: 10303 sec: 0 MATM istep1: 1487 idate: 10304 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 3/ 4 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 3/ 4 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347827059008E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5832.2044 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347827058519E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.465001196617E+05 The minimum dzt is 4.761148062082E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 39.6390 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.761148061011E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.927799301371E+03 The minimum T is -2.047784900721E+00 deg C at (i,j,k) = ( 241, 2, 29), (lon,lat,dpt) = ( -39.5000, -77.6297, 812.7816 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 5.025924228013E+01 m) yyyy/mm/dd hh:mm:ss = 1/ 3/ 4 0: 0: 0 Tracer integrals for temp The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.201822633978E+04 And the number of cells in the column are kmt = 29 The maximum T is 3.092726126242E+01 deg C at (i,j,k) = ( 60, 92, 4), (lon,lat,dpt) = ( -220.5000, -17.1490, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.062513287499E+05, 7.606978203305E+04, 1.015031115355E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.050510069418E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68644705294977637E+00 Variance temp = 2.02293006449635406E+01 |dT/dt| temp = 1.47697422902844977E+00 Total temp = 1.96725563712251306E+25 yyyy/mm/dd hh:mm:ss = 1/ 3/ 4 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 3/ 4 0: 0: 0 Tracer integrals for salt The maximum S is 4.062825852974E+01 psu at (i,j,k) = ( 315, 195, 2), (lon,lat,dpt) = ( 34.5000, 27.5082, 15.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 9.997906649131E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.034692669566E+04 And the number of cells in the column are kmt = 5 The minimum S is 6.294242996622E+00 psu at (i,j,k) = ( 304, 235, 1), (lon,lat,dpt) = ( 23.5000, 59.9708, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.564647372818E+04, 5.780019800035E+04, 9.860766451537E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.020509895708E+04 And the number of cells in the column are kmt = 5 Average salt = 3.47230777904378058E+01 Variance salt = 1.45842254566105112E-01 |dT/dt| salt = 1.57506577594768493E-01 Total salt = 4.64161643058345411E+19 yyyy/mm/dd hh:mm:ss = 1/ 3/ 4 0: 0: 0 The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.870951215155E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021675474062E+04 yyyy/mm/dd hh:mm:ss = 1/ 3/ 4 0: 0: 0 Tracer integrals for age_global And the number of cells in the column are kmt = 12 The maximum age_global is 1.696326717266E-01 yr at (i,j,k) = ( 338, 281, 7), (lon,lat,dpt) = ( 65.6026, 71.5268, 65.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.693914597147E+04, 2.592186576923E+04, 9.816812878459E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.016048005121E+04 And the number of cells in the column are kmt = 9 Average age_global = 1.65976931301155761E-01 Variance age_global = 5.35449815447779087E-04 |dT/dt| age_global = 9.98386030972350930E-02 Total age_global = 2.21870093450478158E+20 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 3/ 4 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.69750046937465671E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -2.31712724679578086E+00 dbar Global max surface height on tracer cells (tau) = 1.00334698661003707E+00 m Global min surface height on tracer cells (tau) = -3.63092261868359634E+00 m Area average surface height on tracer cells (tau) = -8.39692086342645576E-03 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -3.03410980773474219E+12 m^3 Total Mass change = -2.24542861575092188E+12 kg Mass of ocean tracer cells (tau) = 1.33675259393672846E+21 kg Mass from sources = 1.90734863281250000E-04 kg Mass from eta smoothing = 1.90734863281250000E-04 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -5.16116588958246484E+12 kg Mass of river runoff liquid water input = 4.66933361922966421E+08 kg Mass of sea ice melt input = 2.91527034108065771E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = -6.11038391530513763E+02 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96725563712251306E+25 J Total heat change of full system for (taup1-taum1) = 5.92337306741541110E+19 J Total heat input to ocean referenced to 0degC = 5.92336651298814853E+19 J Heat input via surface heat fluxes = 5.93588567190894838E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -2.16701786591984000E+17 J Heat input via river runoff = 3.10535951174316719E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 9.14791437888681920E+16 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = 1.48736832812500000E+06 J Heat input via eta_t smooth = 0.00000000000000000E+00 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 5.92337306741541110E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 6.55442711382956719E+13 J Mismatch converted to a surface flux = 5.03872902757724914E-05 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161643058345411E+19 kg Total tracer change in system for (taup1-taum1) = 1.16610707460844727E+10 kg Total tracer input to ocean = 1.16610707480677299E+10 kg Tracer input via surface fluxes = 1.16610707480677338E+10 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = -7.27514314651489258E+00 kg Tracer input via eta_t smoother = -3.33786010742187500E-06 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 1.17178251774056644E+10 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = 5.31764146125936499E+00 kg Mismatch converted to a surface flux = 4.08794756944681238E-18 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 1.65976931301155761E-01 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066449491029312E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758110839815344E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758110839815344E-04 yr Age input via sources in th_tendency, or errors = 8.67014870368508351E-21 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.11174889804011183E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -2.58322103580415473E-06 yr Mismatch converted to a surface flux = -6.26688608955141343E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 1511 idate: 10305 sec: 0 MATM istep1: 1535 idate: 10306 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 3/ 6 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 3/ 6 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347839382569E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5832.2259 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347839382080E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.465013305103E+05 The minimum dzt is 4.760131799405E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 39.6305 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.760131798334E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.926669101561E+03 The minimum T is -2.045500580053E+00 deg C at (i,j,k) = ( 241, 2, 29), (lon,lat,dpt) = ( -39.5000, -77.6297, 812.7816 m) yyyy/mm/dd hh:mm:ss = 1/ 3/ 6 0: 0: 0 Tracer integrals for temp The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 5.025597999123E+01 m) The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.201490076221E+04 And the number of cells in the column are kmt = 29 The maximum T is 3.095878833691E+01 deg C at (i,j,k) = ( 60, 92, 4), (lon,lat,dpt) = ( -220.5000, -17.1490, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.062513287499E+05, 7.606978203305E+04, 1.015453903586E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.051049065413E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68652579802874936E+00 Variance temp = 2.02347939324872677E+01 |dT/dt| temp = 1.44127545260375234E+00 Total temp = 1.96729749943555803E+25 yyyy/mm/dd hh:mm:ss = 1/ 3/ 6 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 3/ 6 0: 0: 0 Tracer integrals for salt The maximum S is 4.063260613836E+01 psu at (i,j,k) = ( 315, 195, 3), (lon,lat,dpt) = ( 34.5000, 27.5082, 25.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 9.998744750729E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.034991853888E+04 And the number of cells in the column are kmt = 5 The minimum S is 6.291161290244E+00 psu at (i,j,k) = ( 304, 235, 1), (lon,lat,dpt) = ( 23.5000, 59.9708, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.564647372818E+04, 5.780019800035E+04, 9.816550765097E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.016079465979E+04 And the number of cells in the column are kmt = 5 Average salt = 3.47230810235108365E+01 Variance salt = 1.45817781887672027E-01 |dT/dt| salt = 1.58182540476524414E-01 Total salt = 4.64161648611561308E+19 yyyy/mm/dd hh:mm:ss = 1/ 3/ 6 0: 0: 0 The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.867352144860E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021270645023E+04 yyyy/mm/dd hh:mm:ss = 1/ 3/ 6 0: 0: 0 Tracer integrals for age_global And the number of cells in the column are kmt = 12 The maximum age_global is 1.751083733022E-01 yr at (i,j,k) = ( 338, 281, 7), (lon,lat,dpt) = ( 65.6026, 71.5268, 65.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.693914597147E+04, 2.592186576923E+04, 9.817378104652E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.016103771693E+04 And the number of cells in the column are kmt = 9 Average age_global = 1.71304169256583594E-01 Variance age_global = 5.75144401655895698E-04 |dT/dt| age_global = 9.89430958056912169E-02 Total age_global = 2.28991274024134050E+20 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 3/ 6 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.71330508462600428E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -2.27237969556720953E+00 dbar Global max surface height on tracer cells (tau) = 1.02110781588606336E+00 m Global min surface height on tracer cells (tau) = -3.68135070474885273E+00 m Area average surface height on tracer cells (tau) = -8.68696748300205532E-03 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -3.13891409343281250E+12 m^3 Total Mass change = -2.28580239395972852E+12 kg Mass of ocean tracer cells (tau) = 1.33675248546429272E+21 kg Mass from sources = 1.37329101562500000E-04 kg Mass from eta smoothing = 1.37329101562500000E-04 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -5.19381867524647852E+12 kg Mass of river runoff liquid water input = 4.61959502710304379E+08 kg Mass of sea ice melt input = 2.90755432171342676E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = 7.06128004789352417E+01 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96729749943555803E+25 J Total heat change of full system for (taup1-taum1) = 4.65832072862046208E+19 J Total heat input to ocean referenced to 0degC = 4.65831568535115858E+19 J Heat input via surface heat fluxes = 4.67383860657521705E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -2.25647751966852544E+17 J Heat input via river runoff = 3.03911691118477031E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 7.03881485571549120E+16 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = 1.74862829687500000E+06 J Heat input via eta_t smooth = 4.00000000000000000E+00 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 4.65832072862046208E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 5.04326912863797031E+13 J Mismatch converted to a surface flux = 3.87702328686130473E-05 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161648611561308E+19 kg Total tracer change in system for (taup1-taum1) = 1.16302065084636230E+10 kg Total tracer input to ocean = 1.16302064943681526E+10 kg Tracer input via surface fluxes = 1.16302064943681564E+10 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = 1.80807876586914063E+00 kg Tracer input via eta_t smoother = -3.81469726562500000E-06 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 1.16868107235403156E+10 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = 1.23471943978195178E+01 kg Mismatch converted to a surface flux = 9.49193052893411845E-18 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 1.71304169256583622E-01 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066434152690496E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758108599964190E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758108599964190E-04 yr Age input via sources in th_tendency, or errors = -2.04904238777783198E-20 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.11224413546828500E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -2.53369505313569101E-06 yr Mismatch converted to a surface flux = -6.14673621172272944E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 1559 idate: 10307 sec: 0 MATM istep1: 1583 idate: 10308 sec: 0 yyyy/mm/dd hh:mm:ss = 1/ 3/ 8 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 3/ 8 0: 0: 0 From ocean_tracer_diag, dzt_min_max information The maximum dzt is 3.347835617141E+02 metre at (i,j,k) = ( 67, 190, 50), (lon,lat,dpt) = ( -213.5000, 22.7449, 5832.2194 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.025479254585E+05, 1.003388466505E+05, 3.347835616653E+02 m) The number of cells in the column are kmt = 50 The grid dimensions (dst,rho_dzt) = 3.347304687500E+02, 3.465009545151E+05 The minimum dzt is 4.767707716345E+00 metre at (i,j,k) = ( 40, 288, 5), (lon,lat,dpt) = ( -260.7610, 76.8858, 39.6936 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.087078898180E+04, 3.821797945364E+04, 4.767707715273E+00 m) And the number of cells in the column are kmt = 5 The grid dimensions (dst,rho_dzt) = 5.111485611302E+00, 4.934202679455E+03 The minimum T is -2.043246262746E+00 deg C at (i,j,k) = ( 241, 2, 29), (lon,lat,dpt) = ( -39.5000, -77.6297, 812.7816 m) yyyy/mm/dd hh:mm:ss = 1/ 3/ 8 0: 0: 0 Tracer integrals for temp The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 5.025689179388E+01 m) The grid dimensions (dst,rho_dzt) = 5.046637552616E+01, 5.201588113743E+04 And the number of cells in the column are kmt = 29 The maximum T is 3.080551170108E+01 deg C at (i,j,k) = ( 60, 92, 4), (lon,lat,dpt) = ( -220.5000, -17.1490, 35.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 1.062513287499E+05, 7.606978203305E+04, 1.015109152330E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.050693417834E+04 And the number of cells in the column are kmt = 5 Average temp = 3.68653852925184911E+00 Variance temp = 2.02364931946323594E+01 |dT/dt| temp = 1.43050479788761353E+00 Total temp = 1.96730413211380762E+25 yyyy/mm/dd hh:mm:ss = 1/ 3/ 8 0: 0: 0 yyyy/mm/dd hh:mm:ss = 1/ 3/ 8 0: 0: 0 Tracer integrals for salt The maximum S is 4.064081441103E+01 psu at (i,j,k) = ( 315, 195, 3), (lon,lat,dpt) = ( 34.5000, 27.5082, 25.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 9.862374833942E+04, 1.099319682291E+05, 1.001784810379E+01 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.036927678614E+04 And the number of cells in the column are kmt = 5 The minimum S is 6.288325627912E+00 psu at (i,j,k) = ( 304, 235, 1), (lon,lat,dpt) = ( 23.5000, 59.9708, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 5.564647372818E+04, 5.780019800035E+04, 9.855938194919E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.020051564569E+04 And the number of cells in the column are kmt = 5 Average salt = 3.47230842881514405E+01 Variance salt = 1.45803167651592958E-01 |dT/dt| salt = 1.57698212486590300E-01 Total salt = 4.64161654199592468E+19 yyyy/mm/dd hh:mm:ss = 1/ 3/ 8 0: 0: 0 The minimum age_global is 3.000000000000E-12 yr at (i,j,k) = ( 85, 2, 1), (lon,lat,dpt) = ( -195.5000, -77.6297, 5.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 2.382115562586E+04, 2.751611123807E+04, 9.869474673987E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.021506698788E+04 yyyy/mm/dd hh:mm:ss = 1/ 3/ 8 0: 0: 0 Tracer integrals for age_global And the number of cells in the column are kmt = 12 The maximum age_global is 1.805840748777E-01 yr at (i,j,k) = ( 338, 281, 7), (lon,lat,dpt) = ( 65.6026, 71.5268, 65.0000 m) The grid dimensions are (dxt, dyt, dzt) = ( 3.693914597147E+04, 2.592186576923E+04, 9.825435007794E+00 m) The grid dimensions (dst,rho_dzt) = 1.000000000000E+01, 1.016962513699E+04 And the number of cells in the column are kmt = 9 Average age_global = 1.76627027622138222E-01 Variance age_global = 6.17371901832513420E-04 |dT/dt| age_global = 1.00174764928070009E-01 Total age_global = 2.36106598817962787E+20 Mass and tracer change summary (over one timestep): yyyy/mm/dd hh:mm:ss = 1/ 3/ 8 0: 0: 0 ----Single time step diagnostics for volume and mass---- Global max (pbot_t-pbot0) on tracer cells (tau) = 1.72395283894836915E+00 dbar Global min (pbot_t-pbot0) on tracer cells (tau) = -2.25257248499570428E+00 dbar Global max surface height on tracer cells (tau) = 1.02330282972971265E+00 m Global min surface height on tracer cells (tau) = -3.65296228201802231E+00 m Area average surface height on tracer cells (tau) = -8.97999548875117251E-03 m Surface area of k=1 tracer cells = 3.61336001265664000E+14 m^2 Area integral of surface height on tracer cells = -3.24479566128905078E+12 m^3 Total Mass change = -2.27297482623412891E+12 kg Mass of ocean tracer cells (tau) = 1.33675237587686995E+21 kg Mass from sources = 3.81469726562500000E-06 kg Mass from eta smoothing = 3.81469726562500000E-06 kg Mass from pbot smoothing = 0.00000000000000000E+00 kg Mass of precip-evap input = -5.18698383762428516E+12 kg Mass of river runoff liquid water input = 4.48462748631430805E+08 kg Mass of sea ice melt input = 2.91356054930649561E+12 kg Mass of calving land ice input = 0.00000000000000000E+00 kg Mass flux through open boundaries = 0.00000000000000000E+00 kg Mismatch between mass change and water input = -6.64971278369426727E+02 kg ----Single time step diagnostics for tracer temp---- Total heat in ocean at (tau) referenced to 0degC = 1.96730413211380762E+25 J Total heat change of full system for (taup1-taum1) = 4.26074025455531950E+19 J Total heat input to ocean referenced to 0degC = 4.26073511146500342E+19 J Heat input via surface heat fluxes = 4.27760070403313500E+19 J Heat input via bottom heat fluxes = 0.00000000000000000E+00 J Heat input via open boundaries = 0.00000000000000000E+00 J Heat input via precip-evap+melt = -2.40466406199214592E+17 J Heat input via river runoff = 2.91495019928770195E+13 J Heat input via calving land ice = 0.00000000000000000E+00 J Heat input via frazil formation = 7.17813310159102960E+16 J Heat input via sources in the source array = 0.00000000000000000E+00 J Heat input via sources in th_tendency, or errors = 5.67894980468750000E+05 J Heat input via eta_t smooth = -4.00000000000000000E+00 J Heat input via pbot_t smooth = 0.00000000000000000E+00 J d(T*rho*dV) = 4.26074025455531950E+19 J Tracer mismatch: cp*d(rho*dV*T)-input = 5.14309025929370156E+13 J Mismatch converted to a surface flux = 3.95376098183686784E-05 W/m^2 ----Single time step diagnostics for tracer salt---- Total tracer in ocean at time (tau) = 4.64161654199592468E+19 kg Total tracer change in system for (taup1-taum1) = 1.16542313219346924E+10 kg Total tracer input to ocean = 1.16542313061787891E+10 kg Tracer input via surface fluxes = 1.16542313061787872E+10 kg Tracer input via bottom fluxes = 0.00000000000000000E+00 kg Tracer input via open boundaries = 0.00000000000000000E+00 kg Tracer input via precip-evap+melt = 0.00000000000000000E+00 kg Tracer input via river runoff = 0.00000000000000000E+00 kg Tracer input via calving land ice = 0.00000000000000000E+00 kg Tracer input via sources in source array = 0.00000000000000000E+00 kg Tracer input via sources in th_tendency, or errors = -4.37746644020080566E-01 kg Tracer input via eta_t smoother = 2.50339508056640625E-06 kg Tracer input via pbot_t smoother = 0.00000000000000000E+00 kg .001*d(S*rho*dV) = 1.17109524657785473E+10 kg Tracer mismatch: 0.001*d(rho*dV*T)-input = 1.62724643820437187E+01 kg Mismatch converted to a surface flux = 1.25094897247418829E-17 kg/(m^2 sec) ----Single time step diagnostics for tracer age_global---- Total age at (tau) [sum(rho*dV*age)/mass_ocean] = 1.76627027622138222E-01 yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r = 1.52066417081316768E+17 kg*yr dtts*(mass_ocean-mass_k=1)*sec_in_yr_r/mass_taup1 = 1.13758105154019258E-04 yr Total age input to ocean = 0.00000000000000000E+00 yr Age input via surface fluxes = 0.00000000000000000E+00 yr Age input via bottom fluxes = 0.00000000000000000E+00 yr Age input via open boundaries = 0.00000000000000000E+00 yr Age input via precip-evap+melt = 0.00000000000000000E+00 yr Age input via river runoff = 0.00000000000000000E+00 yr Age input via calving land ice = 0.00000000000000000E+00 yr Age input via sources in source array = 1.13758105154019285E-04 yr Age input via sources in th_tendency, or errors = -3.62410521624068916E-20 yr Age input via eta_t smoother = 0.00000000000000000E+00 yr Age input via pbot_t smoother = 0.00000000000000000E+00 yr d(age*rho*vol)/mass_ocean = 1.11075520267882002E-04 yr Age mismatch: [d(rho*dV*age) - dtts*(Mt-M1)]/Mt = -2.68258488613726166E-06 yr Mismatch converted to a surface flux = -6.50794247722633453E-17 1/m^2 Locations (if any) where land cell tracer is non-zero... MATM istep1: 1607 idate: 10309 sec: 0