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MOM_input
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! This file was written by the model and records the non-default parameters used at run-time.
! === module MOM ===
!DIABATIC_FIRST = True ! [Boolean] default = False
! If true, apply diabatic and thermodynamic processes, including buoyancy
! forcing and mass gain or loss, before stepping the dynamics forward.
USE_REGRIDDING = True ! [Boolean] default = False
! If True, use the ALE algorithm (regridding/remapping). If False, use the
! layered isopycnal algorithm.
REMAP_AUXILIARY_VARS = True ! [Boolean] default = False
! If true, apply ALE remapping to all of the auxiliary 3-dimensional variables
! that are needed to reproduce across restarts, similarly to what is already
! being done with the primary state variables. The default should be changed to
! true.
DT = 600.0 ! [s]
! The (baroclinic) dynamics time step. The time-step that is actually used will
! be an integer fraction of the forcing time-step (DT_FORCING in ocean-only mode
! or the coupling timestep in coupled mode.)
DT_THERM = 3600.0 ! [s] default = 600.0
! The thermodynamic and tracer advection time step. Ideally DT_THERM should be
! an integer multiple of DT and less than the forcing or coupling time-step,
! unless THERMO_SPANS_COUPLING is true, in which case DT_THERM can be an integer
! multiple of the coupling timestep. By default DT_THERM is set to DT.
FRAZIL = True ! [Boolean] default = False
! If true, water freezes if it gets too cold, and the accumulated heat deficit
! is returned in the surface state. FRAZIL is only used if
! ENABLE_THERMODYNAMICS is true.
BOUND_SALINITY = True ! [Boolean] default = False
! If true, limit salinity to being positive. (The sea-ice model may ask for more
! salt than is available and drive the salinity negative otherwise.)
C_P = 3992.0 ! [J kg-1 K-1] default = 3991.86795711963
! The heat capacity of sea water, approximated as a constant. This is only used
! if ENABLE_THERMODYNAMICS is true. The default value is from the TEOS-10
! definition of conservative temperature.
CHECK_BAD_SURFACE_VALS = True ! [Boolean] default = False
! If true, check the surface state for ridiculous values.
BAD_VAL_SSH_MAX = 50.0 ! [m] default = 20.0
! The value of SSH above which a bad value message is triggered, if
! CHECK_BAD_SURFACE_VALS is true.
BAD_VAL_SSS_MAX = 75.0 ! [PPT] default = 45.0
! The value of SSS above which a bad value message is triggered, if
! CHECK_BAD_SURFACE_VALS is true.
BAD_VAL_SST_MAX = 55.0 ! [deg C] default = 45.0
! The value of SST above which a bad value message is triggered, if
! CHECK_BAD_SURFACE_VALS is true.
BAD_VAL_SST_MIN = -3.0 ! [deg C] default = -2.1
! The value of SST below which a bad value message is triggered, if
! CHECK_BAD_SURFACE_VALS is true.
! === module MOM_domains ===
REENTRANT_X = False ! [Boolean] default = True
! If true, the domain is zonally reentrant.
NIGLOBAL = 237 !
! The total number of thickness grid points in the x-direction in the physical
! domain. With STATIC_MEMORY_ this is set in MOM_memory.h at compile time.
NJGLOBAL = 277 !
! The total number of thickness grid points in the y-direction in the physical
! domain. With STATIC_MEMORY_ this is set in MOM_memory.h at compile time.
! === module MOM_fixed_initialization ===
INPUTDIR = "INPUT" ! default = "."
! The directory in which input files are found.
! === module MOM_grid_init ===
GRID_CONFIG = "mosaic" !
! A character string that determines the method for defining the horizontal
! grid. Current options are:
! mosaic - read the grid from a mosaic (supergrid)
! file set by GRID_FILE.
! cartesian - use a (flat) Cartesian grid.
! spherical - use a simple spherical grid.
! mercator - use a Mercator spherical grid.
GRID_FILE = "ocean_hgrid.nc" !
! Name of the file from which to read horizontal grid data.
TOPO_CONFIG = "file" !
! This specifies how bathymetry is specified:
! file - read bathymetric information from the file
! specified by (TOPO_FILE).
! flat - flat bottom set to MAXIMUM_DEPTH.
! bowl - an analytically specified bowl-shaped basin
! ranging between MAXIMUM_DEPTH and MINIMUM_DEPTH.
! spoon - a similar shape to 'bowl', but with an vertical
! wall at the southern face.
! halfpipe - a zonally uniform channel with a half-sine
! profile in the meridional direction.
! bbuilder - build topography from list of functions.
! benchmark - use the benchmark test case topography.
! Neverworld - use the Neverworld test case topography.
! DOME - use a slope and channel configuration for the
! DOME sill-overflow test case.
! ISOMIP - use a slope and channel configuration for the
! ISOMIP test case.
! DOME2D - use a shelf and slope configuration for the
! DOME2D gravity current/overflow test case.
! Kelvin - flat but with rotated land mask.
! seamount - Gaussian bump for spontaneous motion test case.
! dumbbell - Sloshing channel with reservoirs on both ends.
! shelfwave - exponential slope for shelfwave test case.
! Phillips - ACC-like idealized topography used in the Phillips config.
! dense - Denmark Strait-like dense water formation and overflow.
! USER - call a user modified routine.
TOPO_FILE = "ocean_topog.nc" ! default = "topog.nc"
! The file from which the bathymetry is read.
MINIMUM_DEPTH = 5.0 ! [m] default = 0.0
! If MASKING_DEPTH is unspecified, then anything shallower than MINIMUM_DEPTH is
! assumed to be land and all fluxes are masked out. If MASKING_DEPTH is
! specified, then all depths shallower than MINIMUM_DEPTH but deeper than
! MASKING_DEPTH are rounded to MINIMUM_DEPTH.
MASKING_DEPTH = 1.0 ! [m] default = -9999.0
! The depth below which to mask points as land points, for which all fluxes are
! zeroed out. MASKING_DEPTH is ignored if it has the special default value.
MAXIMUM_DEPTH = 6500.0 ! [m]
! The maximum depth of the ocean.
! === module MOM_open_boundary ===
! Controls where open boundaries are located, what kind of boundary condition to impose, and what data to apply,
! if any.
OBC_NUMBER_OF_SEGMENTS = 4 ! default = 0
! The number of open boundary segments.
OBC_FREESLIP_VORTICITY = False ! [Boolean] default = True
! If true, sets the normal gradient of tangential velocity to zero in the
! relative vorticity on open boundaries. This cannot be true if another
! OBC_XXX_VORTICITY option is True.
OBC_COMPUTED_VORTICITY = True ! [Boolean] default = False
! If true, uses the external values of tangential velocity in the relative
! vorticity on open boundaries. This cannot be true if another OBC_XXX_VORTICITY
! option is True.
OBC_FREESLIP_STRAIN = False ! [Boolean] default = True
! If true, sets the normal gradient of tangential velocity to zero in the strain
! use in the stress tensor on open boundaries. This cannot be true if another
! OBC_XXX_STRAIN option is True.
OBC_COMPUTED_STRAIN = True ! [Boolean] default = False
! If true, sets the normal gradient of tangential velocity to zero in the strain
! use in the stress tensor on open boundaries. This cannot be true if another
! OBC_XXX_STRAIN option is True.
OBC_ZERO_BIHARMONIC = True ! [Boolean] default = False
! If true, zeros the Laplacian of flow on open boundaries in the biharmonic
! viscosity term.
OBC_RAMP_TIMESCALE = 2.0 ! [days] default = 1.0
! If RAMP_OBCS is true, this sets the ramping timescale.
OBC_TIDE_N_CONSTITUENTS = 10 ! default = 0
! Number of tidal constituents being added to the open boundary.
OBC_SEGMENT_001 = "J=N,I=N:0,FLATHER,ORLANSKI,NUDGED,ORLANSKI_TAN,NUDGED_TAN" !
! Documentation needs to be dynamic?????
OBC_SEGMENT_001_VELOCITY_NUDGING_TIMESCALES = 3.0, 360.0 ! [days] default = 0.0
! Timescales in days for nudging along a segment, for inflow, then outflow.
! Setting both to zero should behave like SIMPLE obcs for the baroclinic
! velocities.
OBC_SEGMENT_002 = "I=0,J=N:0,FLATHER,ORLANSKI,NUDGED,ORLANSKI_TAN,NUDGED_TAN" !
! Documentation needs to be dynamic?????
OBC_SEGMENT_002_VELOCITY_NUDGING_TIMESCALES = 3.0, 360.0 ! [days] default = 0.0
! Timescales in days for nudging along a segment, for inflow, then outflow.
! Setting both to zero should behave like SIMPLE obcs for the baroclinic
! velocities.
OBC_SEGMENT_003 = "J=0,I=0:N,FLATHER,ORLANSKI,NUDGED,ORLANSKI_TAN,NUDGED_TAN" !
! Documentation needs to be dynamic?????
OBC_SEGMENT_003_VELOCITY_NUDGING_TIMESCALES = 3.0, 360.0 ! [days] default = 0.0
! Timescales in days for nudging along a segment, for inflow, then outflow.
! Setting both to zero should behave like SIMPLE obcs for the baroclinic
! velocities.
OBC_SEGMENT_004 = "I=N,J=0:N,FLATHER,ORLANSKI,NUDGED,ORLANSKI_TAN,NUDGED_TAN" !
! Documentation needs to be dynamic?????
OBC_SEGMENT_004_VELOCITY_NUDGING_TIMESCALES = 3.0, 360.0 ! [days] default = 0.0
! Timescales in days for nudging along a segment, for inflow, then outflow.
! Setting both to zero should behave like SIMPLE obcs for the baroclinic
! velocities.
OBC_TRACER_RESERVOIR_LENGTH_SCALE_OUT = 3000.0 ! [m] default = 0.0
! An effective length scale for restoring the tracer concentration at the
! boundaries to externally imposed values when the flow is exiting the domain.
OBC_TRACER_RESERVOIR_LENGTH_SCALE_IN = 3000.0 ! [m] default = 0.0
! An effective length scale for restoring the tracer concentration at the
! boundaries to values from the interior when the flow is entering the domain.
BRUSHCUTTER_MODE = True ! [Boolean] default = False
! If true, read external OBC data on the supergrid.
OBC_REMAPPING_USE_OM4_SUBCELLS = False ! [Boolean] default = True
! If true, use the OM4 remapping-via-subcells algorithm for neutral diffusion.
! See REMAPPING_USE_OM4_SUBCELLS for more details. We recommend setting this
! option to false.
OBC_TIDE_CONSTITUENTS = "M2,S2,N2,K2,K1,O1,P1,Q1,MM,MF" !
! Names of tidal constituents being added to the open boundaries.
OBC_TIDE_ADD_EQ_PHASE = True ! [Boolean] default = False
! If true, add the equilibrium phase argument to the specified tidal phases.
OBC_TIDE_ADD_NODAL = True ! [Boolean] default = False
! If true, include 18.6 year nodal modulation in the boundary tidal forcing.
OBC_TIDE_REF_DATE = 1980, 1, 1 !
! Reference date to use for tidal calculations and equilibrium phase.
OBC_TIDE_NODAL_REF_DATE = 2011, 7, 2 ! default = 0
! Fixed reference date to use for nodal modulation of boundary tides.
! === module MOM_verticalGrid ===
! Parameters providing information about the vertical grid.
NK = 75 ! [nondim]
! The number of model layers.
! === module MOM_EOS ===
EQN_OF_STATE = "WRIGHT_FULL" ! default = "WRIGHT"
! EQN_OF_STATE determines which ocean equation of state should be used.
! Currently, the valid choices are "LINEAR", "UNESCO", "JACKETT_MCD", "WRIGHT",
! "WRIGHT_REDUCED", "WRIGHT_FULL", "NEMO", "ROQUET_RHO", "ROQUET_SPV" and
! "TEOS10". This is only used if USE_EOS is true.
DTFREEZE_DP = -7.75E-08 ! [degC Pa-1] default = 0.0
! When TFREEZE_FORM=LINEAR, this is the derivative of the freezing potential
! temperature with pressure.
! === module MOM_tracer_flow_control ===
! === module MOM_boundary_update ===
! === module segment_tracer_registry_init ===
! === module MOM_coord_initialization ===
COORD_CONFIG = "ALE" ! default = "none"
! This specifies how layers are to be defined:
! ALE or none - used to avoid defining layers in ALE mode
! file - read coordinate information from the file
! specified by (COORD_FILE).
! BFB - Custom coords for buoyancy-forced basin case
! based on SST_S, T_BOT and DRHO_DT.
! linear - linear based on interfaces not layers
! layer_ref - linear based on layer densities
! ts_ref - use reference temperature and salinity
! ts_range - use range of temperature and salinity
! (T_REF and S_REF) to determine surface density
! and GINT calculate internal densities.
! gprime - use reference density (RHO_0) for surface
! density and GINT calculate internal densities.
! ts_profile - use temperature and salinity profiles
! (read from COORD_FILE) to set layer densities.
! USER - call a user modified routine.
REGRIDDING_COORDINATE_MODE = "Z*" ! default = "LAYER"
! Coordinate mode for vertical regridding. Choose among the following
! possibilities: LAYER - Isopycnal or stacked shallow water layers
! ZSTAR, Z* - stretched geopotential z*
! SIGMA_SHELF_ZSTAR - stretched geopotential z* ignoring shelf
! SIGMA - terrain following coordinates
! RHO - continuous isopycnal
! HYCOM1 - HyCOM-like hybrid coordinate
! HYBGEN - Hybrid coordinate from the Hycom hybgen code
! ADAPTIVE - optimize for smooth neutral density surfaces
ALE_COORDINATE_CONFIG = "FILE:vgrid_75_2m.nc,dz" ! default = "UNIFORM"
! Determines how to specify the coordinate resolution. Valid options are:
! PARAM - use the vector-parameter ALE_RESOLUTION
! UNIFORM[:N] - uniformly distributed
! FILE:string - read from a file. The string specifies
! the filename and variable name, separated
! by a comma or space, e.g. FILE:lev.nc,dz
! or FILE:lev.nc,interfaces=zw
! WOA09[:N] - the WOA09 vertical grid (approximately)
! FNC1:string - FNC1:dz_min,H_total,power,precision
! HYBRID:string - read from a file. The string specifies
! the filename and two variable names, separated
! by a comma or space, for sigma-2 and dz. e.g.
! HYBRID:vgrid.nc,sigma2,dz
!ALE_RESOLUTION = 4*2.0, 2*2.01, 2.02, 2.03, 2.05, 2.08, 2.11, 2.15, 2.2, 2.27, 2.34, 2.44, 2.55, 2.69, 2.85, 3.04, 3.27, 3.54, 3.85, 4.22, 4.66, 5.18, 5.79, 6.52, 7.37, 8.37, 9.55, 10.94, 12.57, 14.48, 16.72, 19.33, 22.36, 25.87, 29.91, 34.53, 39.79, 45.72, 52.37, 59.76, 67.89, 76.74, 86.29, 96.47, 107.2, 118.35, 129.81, 141.42, 153.01, 164.41, 175.47, 186.01, 195.9, 205.01, 213.27, 220.6, 226.99, 232.43, 236.96, 240.63, 243.52, 245.72, 247.33, 248.45, 249.18, 249.62, 249.86, 249.96, 249.99, 2*250.0 ! [m]
! The distribution of vertical resolution for the target
! grid used for Eulerian-like coordinates. For example,
! in z-coordinate mode, the parameter is a list of level
! thicknesses (in m). In sigma-coordinate mode, the list
! is of non-dimensional fractions of the water column.
MIN_THICKNESS = 1.0E-06 ! [m] default = 0.001
! When regridding, this is the minimum layer thickness allowed.
REMAPPING_SCHEME = "PPM_H4" ! default = "PLM"
! This sets the reconstruction scheme used for vertical remapping for all
! variables. It can be one of the following schemes:
! PCM (1st-order accurate)
! PLM (2nd-order accurate)
! PLM_HYBGEN (2nd-order accurate)
! PPM_H4 (3rd-order accurate)
! PPM_IH4 (3rd-order accurate)
! PPM_HYBGEN (3rd-order accurate)
! WENO_HYBGEN (3rd-order accurate)
! PQM_IH4IH3 (4th-order accurate)
! PQM_IH6IH5 (5th-order accurate)
REMAPPING_USE_OM4_SUBCELLS = False ! [Boolean] default = True
! This selects the remapping algorithm used in OM4 that does not use the full
! reconstruction for the top- and lower-most sub-layers, but instead assumes
! they are always vanished (untrue) and so just uses their edge values. We
! recommend setting this option to false.
! === module MOM_state_initialization ===
THICKNESS_CONFIG = "coord" ! default = "uniform"
! A string that determines how the initial layer thicknesses are specified for a
! new run:
! file - read interface heights from the file specified
! by (THICKNESS_FILE).
! thickness_file - read thicknesses from the file specified
! by (THICKNESS_FILE).
! mass_file - read thicknesses in units of mass per unit area from the file
! specified by (THICKNESS_FILE).
! coord - determined by ALE coordinate.
! uniform - uniform thickness layers evenly distributed
! between the surface and MAXIMUM_DEPTH.
! list - read a list of positive interface depths.
! DOME - use a slope and channel configuration for the
! DOME sill-overflow test case.
! ISOMIP - use a configuration for the
! ISOMIP test case.
! benchmark - use the benchmark test case thicknesses.
! Neverworld - use the Neverworld test case thicknesses.
! search - search a density profile for the interface
! densities. This is not yet implemented.
! circle_obcs - the circle_obcs test case is used.
! DOME2D - 2D version of DOME initialization.
! adjustment2d - 2D lock exchange thickness ICs.
! sloshing - sloshing gravity thickness ICs.
! seamount - no motion test with seamount ICs.
! dumbbell - sloshing channel ICs.
! soliton - Equatorial Rossby soliton.
! rossby_front - a mixed layer front in thermal wind balance.
! USER - call a user modified routine.
TS_CONFIG = "file" !
! A string that determines how the initial temperatures and salinities are
! specified for a new run:
! file - read velocities from the file specified
! by (TS_FILE).
! fit - find the temperatures that are consistent with
! the layer densities and salinity S_REF.
! TS_profile - use temperature and salinity profiles
! (read from TS_FILE) to set layer densities.
! benchmark - use the benchmark test case T & S.
! linear - linear in logical layer space.
! DOME2D - 2D DOME initialization.
! ISOMIP - ISOMIP initialization.
! adjustment2d - 2d lock exchange T/S ICs.
! sloshing - sloshing mode T/S ICs.
! seamount - no motion test with seamount ICs.
! dumbbell - sloshing channel ICs.
! rossby_front - a mixed layer front in thermal wind balance.
! SCM_CVMix_tests - used in the SCM CVMix tests.
! USER - call a user modified routine.
TS_FILE = "SODA3_sept.nc" !
! The initial condition file for temperature.
TEMP_IC_VAR = "temp" ! default = "PTEMP"
! The initial condition variable for potential temperature.
SALT_IC_VAR = "salt" ! default = "SALT"
! The initial condition variable for salinity.
DEPRESS_INITIAL_SURFACE = True ! [Boolean] default = False
! If true, depress the initial surface to avoid huge tsunamis when a large
! surface pressure is applied.
SURFACE_HEIGHT_IC_FILE = "SODA3_sept.nc" !
! The initial condition file for the surface height.
SURFACE_HEIGHT_IC_VAR = "ssh" ! default = "SSH"
! The initial condition variable for the surface height.
!VELOCITY_CONFIG = "file"
!VELOCITY_FILE = "SODA3_sept.nc"
!SPONGE = True ! [Boolean] default = False
! If true, sponges may be applied anywhere in the domain. The exact location and
! properties of those sponges are specified via SPONGE_CONFIG.
!SPONGE_DAMPING_FILE = "Bering_idamp.nc" !
! The name of the file with the sponge damping rates.
!SPONGE_STATE_FILE = "bering_soda_mnClim_2011-2012.nc" ! default = "Bering_idamp.nc"
! The name of the file with the state to damp toward.
!SPONGE_PTEMP_VAR = "temp" ! default = "PTEMP"
! The name of the potential temperature variable in SPONGE_STATE_FILE.
!SPONGE_SALT_VAR = "salt" ! default = "SALT"
! The name of the salinity variable in SPONGE_STATE_FILE.
!SPONGE_UV = True ! [Boolean] default = False
! Apply sponges in u and v, in addition to tracers.
!SPONGE_UV_STATE_FILE = "bering_soda_mnClim_2011-2012.nc" ! default = "Bering_idamp.nc"
! The name of the file with the state to damp UV toward.
!SPONGE_U_VAR = "u" ! default = "UVEL"
! The name of the zonal velocity variable in SPONGE_UV_STATE_FILE.
!SPONGE_V_VAR = "v" ! default = "VVEL"
! The name of the vertical velocity variable in SPONGE_UV_STATE_FILE.
!SPONGE_IDAMP_U_var = "Idamp_u" ! default = "Idamp"
! The name of the inverse damping rate variable in SPONGE_UV_DAMPING_FILE for
! the velocities.
!SPONGE_IDAMP_V_var = "Idamp_v" ! default = "Idamp"
! The name of the inverse damping rate variable in SPONGE_UV_DAMPING_FILE for
! the velocities.
!INTERPOLATE_SPONGE_TIME_SPACE = True
! === module MOM_sponge ===
SPONGE_DATA_ONGRID = True ! [Boolean] default = False
! When defined, the incoming sponge data are assumed to be on the model grid
OBC_SEGMENT_001_DATA = "U=file:OBC_whole.nc(u),V=file:OBC_whole.nc(v),SSH=file:OBC_whole.nc(zeta),TEMP=file:OBC_whole.nc(temp),SALT=file:OBC_whole.nc(salt),Uamp=file:tu_001.nc(uamp),Uphase=file:tu_001.nc(uphase),Vamp=file:tu_001.nc(vamp),Vphase=file:tu_001.nc(vphase),SSHamp=file:tz_001.nc(zamp),SSHphase=file:tz_001.nc(zphase)" !
! OBC segment docs
OBC_SEGMENT_002_DATA = "U=file:OBC.nc(u),V=file:OBC.nc(v),SSH=file:OBC.nc(zeta),TEMP=file:OBC.nc(temp),SALT=file:OBC.nc(salt),Uamp=file:tu_002.nc(uamp),Uphase=file:tu_002.nc(uphase),Vamp=file:tu_002.nc(vamp),Vphase=file:tu_002.nc(vphase),SSHamp=file:tz_002.nc(zamp),SSHphase=file:tz_002.nc(zphase)" !
! OBC segment docs
OBC_SEGMENT_003_DATA = "U=file:OBC.nc(u),V=file:OBC.nc(v),SSH=file:OBC.nc(zeta),TEMP=file:OBC.nc(temp),SALT=file:OBC.nc(salt),Uamp=file:tu_003.nc(uamp),Uphase=file:tu_003.nc(uphase),Vamp=file:tu_003.nc(vamp),Vphase=file:tu_003.nc(vphase),SSHamp=file:tz_003.nc(zamp),SSHphase=file:tz_003.nc(zphase)" !
! OBC segment docs
OBC_SEGMENT_004_DATA = "U=file:OBC_whole.nc(u),V=file:OBC_whole.nc(v),SSH=file:OBC_whole.nc(zeta),TEMP=file:OBC_whole.nc(temp),SALT=file:OBC_whole.nc(salt),Uamp=file:tu_004.nc(uamp),Uphase=file:tu_004.nc(uphase),Vamp=file:tu_004.nc(vamp),Vphase=file:tu_004.nc(vphase),SSHamp=file:tz_004.nc(zamp),SSHphase=file:tz_004.nc(zphase)" !
! OBC segment docs
! === module MOM_diag_mediator ===
DIAG_REMAPPING_USE_OM4_SUBCELLS = False ! [Boolean] default = True
! If true, use the OM4 remapping-via-subcells algorithm for diagnostics. See
! REMAPPING_USE_OM4_SUBCELLS for details. We recommend setting this option to
! false.
! === module MOM_lateral_mixing_coeffs ===
USE_VARIABLE_MIXING = True ! [Boolean] default = False
! If true, the variable mixing code will be called. This allows diagnostics to
! be created even if the scheme is not used. If KHTR_SLOPE_CFF>0 or
! KhTh_Slope_Cff>0, this is set to true regardless of what is in the parameter
! file.
USE_STORED_SLOPES = True ! [Boolean] default = False
! If true, the isopycnal slopes are calculated once and stored for re-use. This
! uses more memory but avoids calling the equation of state more times than
! should be necessary.
EBT_REMAPPING_USE_OM4_SUBCELLS = False ! [Boolean] default = True
! If true, use the OM4 remapping-via-subcells algorithm for calculating EBT
! structure. See REMAPPING_USE_OM4_SUBCELLS for details. We recommend setting
! this option to false.
! === module MOM_set_visc ===
CHANNEL_DRAG = True ! [Boolean] default = False
! If true, the bottom drag is exerted directly on each layer proportional to the
! fraction of the bottom it overlies.
PRANDTL_TURB = 1.25 ! [nondim] default = 1.0
! The turbulent Prandtl number applied to shear instability.
HBBL = 10.0 ! [m]
! The thickness of a bottom boundary layer with a viscosity increased by
! KV_EXTRA_BBL if BOTTOMDRAGLAW is not defined, or the thickness over which
! near-bottom velocities are averaged for the drag law if BOTTOMDRAGLAW is
! defined but LINEAR_DRAG is not.
CDRAG = 0.0025 ! [nondim] default = 0.003
! CDRAG is the drag coefficient relating the magnitude of the velocity field to
! the bottom stress. CDRAG is only used if BOTTOMDRAGLAW is defined.
DRAG_BG_VEL = 0.001 ! [m s-1] default = 0.0
! DRAG_BG_VEL is either the assumed bottom velocity (with LINEAR_DRAG) or an
! unresolved velocity that is combined with the resolved velocity to estimate
! the velocity magnitude. DRAG_BG_VEL is only used when BOTTOMDRAGLAW is
! defined.
BBL_THICK_MIN = 0.1 ! [m] default = 0.0
! The minimum bottom boundary layer thickness that can be used with
! BOTTOMDRAGLAW. This might be Kv/(cdrag*drag_bg_vel) to give Kv as the minimum
! near-bottom viscosity.
KV = 0.0 ! [m2 s-1]
! The background kinematic viscosity in the interior. The molecular value, ~1e-6
! m2 s-1, may be used.
! === module MOM_thickness_diffuse ===
KHTH_MAX_CFL = 0.1 ! [nondimensional] default = 0.8
! The maximum value of the local diffusive CFL ratio that is permitted for the
! thickness diffusivity. 1.0 is the marginally unstable value in a pure layered
! model, but much smaller numbers (e.g. 0.1) seem to work better for ALE-based
! models.
! === module MOM_porous_barriers ===
! === module MOM_dynamics_split_RK2 ===
TIDES = True ! [Boolean] default = False
! If true, apply tidal momentum forcing.
VISC_REM_BUG = False ! [Boolean] default = True
! If true, visc_rem_[uv] in split mode is incorrectly calculated or accounted
! for in three places. This parameter controls the defaults of three individual
! flags, VISC_REM_TIMESTEP_FIX in MOM_dynamics_split_RK2(b),
! VISC_REM_BT_WEIGHT_FIX in MOM_barotropic, and VISC_REM_CONT_HVEL_FIX in
! MOM_continuity_PPM. Eventually, the three individual flags should be removed
! after tests and the default of VISC_REM_BUG should be to False.
! === module MOM_continuity_PPM ===
ETA_TOLERANCE = 1.0E-06 ! [m] default = 3.75E-09
! The tolerance for the differences between the barotropic and baroclinic
! estimates of the sea surface height due to the fluxes through each face. The
! total tolerance for SSH is 4 times this value. The default is
! 0.5*NK*ANGSTROM, and this should not be set less than about
! 10^-15*MAXIMUM_DEPTH.
! === module MOM_CoriolisAdv ===
CORIOLIS_EN_DIS = True ! [Boolean] default = False
! If true, two estimates of the thickness fluxes are used to estimate the
! Coriolis term, and the one that dissipates energy relative to the other one is
! used.
CORIOLIS_SCHEME = "SADOURNY75_ENERGY" ! default = "SADOURNY75_ENERGY"
! CORIOLIS_SCHEME selects the discretization for the Coriolis terms. Valid
! values are:
! SADOURNY75_ENERGY - Sadourny, 1975; energy cons.
! ARAKAWA_HSU90 - Arakawa & Hsu, 1990
! SADOURNY75_ENSTRO - Sadourny, 1975; enstrophy cons.
! ARAKAWA_LAMB81 - Arakawa & Lamb, 1981; En. + Enst.
! ARAKAWA_LAMB_BLEND - A blend of Arakawa & Lamb with
! Arakawa & Hsu and Sadourny energy
BOUND_CORIOLIS = True ! [Boolean] default = False
! If true, the Coriolis terms at u-points are bounded by the four estimates of
! (f+rv)v from the four neighboring v-points, and similarly at v-points. This
! option is always effectively false with CORIOLIS_EN_DIS defined and
! CORIOLIS_SCHEME set to SADOURNY75_ENERGY.
! === module MOM_self_attr_load ===
SAL_SCALAR_VALUE = 0.094 ! [m m-1] default = 0.0
! The constant of proportionality between sea surface height (really it should
! be bottom pressure) anomalies and bottom geopotential anomalies. This is only
! used if USE_SAL_SCALAR is true or USE_PREVIOUS_TIDES is true.
! === module MOM_tidal_forcing ===
TIDE_M2 = True ! [Boolean] default = False
! If true, apply tidal momentum forcing at the M2 frequency. This is only used
! if TIDES is true.
TIDE_S2 = True ! [Boolean] default = False
! If true, apply tidal momentum forcing at the S2 frequency. This is only used
! if TIDES is true.
TIDE_N2 = True ! [Boolean] default = False
! If true, apply tidal momentum forcing at the N2 frequency. This is only used
! if TIDES is true.
TIDE_K2 = True ! [Boolean] default = False
! If true, apply tidal momentum forcing at the K2 frequency. This is only used
! if TIDES is true.
TIDE_K1 = True ! [Boolean] default = False
! If true, apply tidal momentum forcing at the K1 frequency. This is only used
! if TIDES is true.
TIDE_O1 = True ! [Boolean] default = False
! If true, apply tidal momentum forcing at the O1 frequency. This is only used
! if TIDES is true.
TIDE_P1 = True ! [Boolean] default = False
! If true, apply tidal momentum forcing at the P1 frequency. This is only used
! if TIDES is true.
TIDE_Q1 = True ! [Boolean] default = False
! If true, apply tidal momentum forcing at the Q1 frequency. This is only used
! if TIDES is true.
TIDE_MF = True ! [Boolean] default = False
! If true, apply tidal momentum forcing at the MF frequency. This is only used
! if TIDES is true.
TIDE_MM = True ! [Boolean] default = False
! If true, apply tidal momentum forcing at the MM frequency. This is only used
! if TIDES is true.
TIDE_REF_DATE = 2011, 1, 1 ! default = 0
! Year,month,day to use as reference date for tidal forcing. If not specified,
! defaults to 0.
TIDE_USE_EQ_PHASE = True ! [Boolean] default = False
! Correct phases by calculating equilibrium phase arguments for TIDE_REF_DATE.
! === module MOM_PressureForce ===
! === module MOM_PressureForce_FV ===
MASS_WEIGHT_IN_PRESSURE_GRADIENT = True ! [Boolean] default = False
! If true, use mass weighting when interpolating T/S for integrals near the
! bathymetry in FV pressure gradient calculations.
! === module MOM_Zanna_Bolton ===
! === module MOM_hor_visc ===
AH_VEL_SCALE = 0.01 ! [m s-1] default = 0.0
! The velocity scale which is multiplied by the cube of the grid spacing to
! calculate the biharmonic viscosity. The final viscosity is the largest of this
! scaled viscosity, the Smagorinsky and Leith viscosities, and AH.
SMAGORINSKY_AH = True ! [Boolean] default = False
! If true, use a biharmonic Smagorinsky nonlinear eddy viscosity.
SMAG_BI_CONST = 0.06 ! [nondim] default = 0.0
! The nondimensional biharmonic Smagorinsky constant, typically 0.015 - 0.06.
FRICTWORK_BUG = False ! [Boolean] default = True
! If true, retain an answer-changing bug in calculating the FrictWork, which
! cancels the h in thickness flux and the h at velocity point. This isnot
! recommended.
USE_LAND_MASK_FOR_HVISC = True ! [Boolean] default = False
! If true, use Use the land mask for the computation of thicknesses
! at velocity locations. This eliminates the dependence on arbitrary
! values over land or outside of the domain. Default is False in order to
! maintain answers with legacy experiments but should be changed to True
! for new experiments.
! === module MOM_vert_friction ===
HMIX_FIXED = 0.9 ! [m]
! The prescribed depth over which the near-surface viscosity and diffusivity are
! elevated when the bulk mixed layer is not used.
KV_ML_INVZ2 = 0.01 ! [m2 s-1] default = 0.0
! An extra kinematic viscosity in a mixed layer of thickness HMIX_FIXED, with
! the actual viscosity scaling as 1/(z*HMIX_FIXED)^2, where z is the distance
! from the surface, to allow for finite wind stresses to be transmitted through
! infinitesimally thin surface layers. This is an older option for numerical
! convenience without a strong physical basis, and its use is now discouraged.
MAXVEL = 6.0 ! [m s-1] default = 3.0E+08
! The maximum velocity allowed before the velocity components are truncated.
! === module MOM_barotropic ===
BOUND_BT_CORRECTION = True ! [Boolean] default = False
! If true, the corrective pseudo mass-fluxes into the barotropic solver are
! limited to values that require less than maxCFL_BT_cont to be accommodated.
BT_PROJECT_VELOCITY = True ! [Boolean] default = False
! If true, step the barotropic velocity first and project out the velocity
! tendency by 1+BEBT when calculating the transport. The default (false) is to
! use a predictor continuity step to find the pressure field, and then to do a
! corrector continuity step using a weighted average of the old and new
! velocities, with weights of (1-BEBT) and BEBT.
BT_NONLIN_STRESS = True ! [Boolean] default = False
! If true, use the full depth of the ocean at the start of the barotropic step
! when calculating the surface stress contribution to the barotropic
! acclerations. Otherwise use the depth based on bathyT.
DYNAMIC_SURFACE_PRESSURE = True ! [Boolean] default = False
! If true, add a dynamic pressure due to a viscous ice shelf, for instance.
TIDAL_SAL_FLATHER = True ! [Boolean] default = False
! If true, then apply adjustments to the external gravity wave speed used with
! the Flather OBC routine consistent with the barotropic solver. This applies to
! cases with tidal forcing using the scalar self-attraction approximation. The
! default is currently False in order to retain previous answers but should be
! set to True for new experiments
BT_STRONG_DRAG = True ! [Boolean] default = False
! If true, use a stronger estimate of the retarding effects of strong bottom
! drag, by making it implicit with the barotropic time-step instead of implicit
! with the baroclinic time-step and dividing by the number of barotropic steps.
LINEARIZED_BT_CORIOLIS = False ! [Boolean] default = True
! If true use the bottom depth instead of the total water column thickness in
! the barotropic Coriolis term calculations.
BEBT = 0.2 ! [nondim] default = 0.1
! BEBT determines whether the barotropic time stepping uses the forward-backward
! time-stepping scheme or a backward Euler scheme. BEBT is valid in the range
! from 0 (for a forward-backward treatment of nonrotating gravity waves) to 1
! (for a backward Euler treatment). In practice, BEBT must be greater than about
! 0.05.
DTBT = -0.9 ! [s or nondim] default = -0.98
! The barotropic time step, in s. DTBT is only used with the split explicit time
! stepping. To set the time step automatically based the maximum stable value
! use 0, or a negative value gives the fraction of the stable value. Setting
! DTBT to 0 is the same as setting it to -0.98. The value of DTBT that will
! actually be used is an integer fraction of DT, rounding down.
! === module MOM_mixed_layer_restrat ===
MIXEDLAYER_RESTRAT = True ! [Boolean] default = False
! If true, a density-gradient dependent re-stratifying flow is imposed in the
! mixed layer. Can be used in ALE mode without restriction but in layer mode can
! only be used if BULKMIXEDLAYER is true.
MLE%
USE_BODNER23 = True ! [Boolean] default = False
! If true, use the Bodner et al., 2023, formulation of the re-stratifying
! mixed-layer restratification parameterization. This only works in ALE mode.
CR = 0.3 ! [nondim] default = 0.0
! The efficiency coefficient in eq 27 of Bodner et al., 2023.
BLD_DECAYING_TFILTER = 8.64E+04 ! [s] default = 0.0
! The time-scale for a running-mean filter applied to the boundary layer depth
! (BLD) when the BLD is shallower than the running mean. A value of 0
! instantaneously sets the running mean to the current value of BLD.
MLD_DECAYING_TFILTER = 2.592E+06 ! [s] default = 0.0
! The time-scale for a running-mean filter applied to the time-filtered BLD,
! when the latter is shallower than the running mean. A value of 0
! instantaneously sets the running mean to the current value filtered BLD.
MIN_WSTAR2 = 1.0E-09 ! [m2 s-2] default = 1.0E-24
! The minimum lower bound to apply to the vertical momentum flux, w'u', in the
! Bodner et al., restratification parameterization. This avoids a
! division-by-zero in the limit when u* and the buoyancy flux are zero. The
! default is less than the molecular viscosity of water times the Coriolis
! parameter a micron away from the equator.
%MLE
FOX_KEMPER_ML_RESTRAT_COEF = 1.0 ! [nondim] default = 0.0
! A nondimensional coefficient that is proportional to the ratio of the
! deformation radius to the dominant lengthscale of the submesoscale mixed layer
! instabilities, times the minimum of the ratio of the mesoscale eddy kinetic
! energy to the large-scale geostrophic kinetic energy or 1 plus the square of
! the grid spacing over the deformation radius, as detailed by Fox-Kemper et al.
! (2010)
MLE_FRONT_LENGTH = 200.0 ! [m] default = 0.0
! If non-zero, is the frontal-length scale used to calculate the upscaling of
! buoyancy gradients that is otherwise represented by the parameter
! FOX_KEMPER_ML_RESTRAT_COEF. If MLE_FRONT_LENGTH is non-zero, it is recommended
! to set FOX_KEMPER_ML_RESTRAT_COEF=1.0.
MLE_USE_PBL_MLD = True ! [Boolean] default = False
! If true, the MLE parameterization will use the mixed-layer depth provided by
! the active PBL parameterization. If false, MLE will estimate a MLD based on a
! density difference with the surface using the parameter MLE_DENSITY_DIFF.
MLE_MLD_DECAY_TIME = 86400.0 ! [s] default = 0.0
! The time-scale for a running-mean filter applied to the mixed-layer depth used
! in the MLE restratification parameterization. When the MLD deepens below the
! current running-mean the running-mean is instantaneously set to the current
! MLD.
! === module MOM_diagnostics ===
INTWAVE_REMAPPING_USE_OM4_SUBCELLS = False ! [Boolean] default = True
! If true, use the OM4 remapping-via-subcells algorithm for calculating EBT
! structure. See REMAPPING_USE_OM4_SUBCELLS for details. We recommend setting
! this option to false.
! === module MOM_diabatic_driver ===
! The following parameters are used for diabatic processes.
USE_LEGACY_DIABATIC_DRIVER = False ! [Boolean] default = True
! If true, use a legacy version of the diabatic subroutine. This is temporary
! and is needed to avoid change in answers.
ENERGETICS_SFC_PBL = True ! [Boolean] default = False
! If true, use an implied energetics planetary boundary layer scheme to
! determine the diffusivity and viscosity in the surface boundary layer.
EPBL_IS_ADDITIVE = False ! [Boolean] default = True
! If true, the diffusivity from ePBL is added to all other diffusivities.
! Otherwise, the larger of kappa-shear and ePBL diffusivities are used.
! === module MOM_set_diffusivity ===
! === module MOM_tidal_mixing ===
! Vertical Tidal Mixing Parameterization
INT_TIDE_DISSIPATION = True ! [Boolean] default = False
! If true, use an internal tidal dissipation scheme to drive diapycnal mixing,
! along the lines of St. Laurent et al. (2002) and Simmons et al. (2004).
INT_TIDE_PROFILE = "POLZIN_09" ! default = "STLAURENT_02"
! INT_TIDE_PROFILE selects the vertical profile of energy dissipation with
! INT_TIDE_DISSIPATION. Valid values are:
! STLAURENT_02 - Use the St. Laurent et al exponential
! decay profile.
! POLZIN_09 - Use the Polzin WKB-stretched algebraic
! decay profile.
INT_TIDE_DECAY_SCALE = 300.0 ! [m] default = 500.0
! The decay scale away from the bottom for tidal TKE with the new coding when
! INT_TIDE_DISSIPATION is used.
H2_FILE = "ocean_topoh2.nc" !
! The path to the file containing the sub-grid-scale topographic roughness
! amplitude with INT_TIDE_DISSIPATION.
BBL_EFFIC = 0.01 ! [nondim] default = 0.2
! The efficiency with which the energy extracted by bottom drag drives BBL
! diffusion. This is only used if BOTTOMDRAGLAW is true.
BBL_MIXING_AS_MAX = False ! [Boolean] default = True
! If true, take the maximum of the diffusivity from the BBL mixing and the other
! diffusivities. Otherwise, diffusivity from the BBL_mixing is simply added.
USE_LOTW_BBL_DIFFUSIVITY = True ! [Boolean] default = False
! If true, uses a simple, imprecise but non-coordinate dependent, model of BBL
! mixing diffusivity based on Law of the Wall. Otherwise, uses the original BBL
! scheme.
LOTW_BBL_ANSWER_DATE = 99991231 ! default = 20190101
! The vintage of the order of arithmetic and expressions in the LOTW_BBL
! calculations. Values below 20240630 recover the original answers, while
! higher values use more accurate expressions. This only applies when
! USE_LOTW_BBL_DIFFUSIVITY is true.
! === module MOM_bkgnd_mixing ===
! Adding static vertical background mixing coefficients
KD = 2.0E-06 ! [m2 s-1] default = 0.0
! The background diapycnal diffusivity of density in the interior. Zero or the
! molecular value, ~1e-7 m2 s-1, may be used.
KD_MIN = 2.0E-07 ! [m2 s-1] default = 2.0E-08
! The minimum diapycnal diffusivity.
KD_MAX = 0.1 ! [m2 s-1] default = -1.0
! The maximum permitted increment for the diapycnal diffusivity from TKE-based
! parameterizations, or a negative value for no limit.
DOUBLE_DIFFUSION = True ! [Boolean] default = False
! If true, increase diffusivites for temperature or salinity based on the
! double-diffusive parameterization described in Large et al. (1994).
! === module MOM_kappa_shear ===
! Parameterization of shear-driven turbulence following Jackson, Hallberg and Legg, JPO 2008
USE_JACKSON_PARAM = True ! [Boolean] default = False
! If true, use the Jackson-Hallberg-Legg (JPO 2008) shear mixing
! parameterization.
MAX_RINO_IT = 25 ! [nondim] default = 50
! The maximum number of iterations that may be used to estimate the Richardson
! number driven mixing.
! === module MOM_diabatic_aux ===
! The following parameters are used for auxiliary diabatic processes.
PRESSURE_DEPENDENT_FRAZIL = True ! [Boolean] default = False
! If true, use a pressure dependent freezing temperature when making frazil. The
! default is false, which will be faster but is inappropriate with ice-shelf
! cavities.
IGNORE_FLUXES_OVER_LAND = True ! [Boolean] default = False
! If true, the model does not check if fluxes are being applied over land
! points. This is needed when the ocean is coupled with ice shelves and sea ice,
! since the sea ice mask needs to be different than the ocean mask to avoid sea
! ice formation under ice shelves. This flag only works when use_ePBL = True.
DO_RIVERMIX = True ! [Boolean] default = False
! If true, apply additional mixing wherever there is runoff, so that it is mixed
! down to RIVERMIX_DEPTH if the ocean is that deep.
RIVERMIX_DEPTH = 10.0 ! [m] default = 0.0
! The depth to which rivers are mixed if DO_RIVERMIX is defined.
! === module MOM_energetic_PBL ===
ML_OMEGA_FRAC = 0.001 ! [nondim] default = 0.0
! When setting the decay scale for turbulence, use this fraction of the absolute
! rotation rate blended with the local value of f, as sqrt((1-of)*f^2 +
! of*4*omega^2).
TKE_DECAY = 0.001 ! [nondim] default = 2.5
! TKE_DECAY relates the vertical rate of decay of the TKE available for
! mechanical entrainment to the natural Ekman depth.
EPBL_MSTAR_SCHEME = "REICHL_H18" ! default = "CONSTANT"
! EPBL_MSTAR_SCHEME selects the method for setting mstar. Valid values are:
! CONSTANT - Use a fixed mstar given by MSTAR
! OM4 - Use L_Ekman/L_Obukhov in the stabilizing limit, as in OM4
! REICHL_H18 - Use the scheme documented in Reichl & Hallberg, 2018.
MSTAR_CAP = 10.0 ! [nondim] default = -1.0
! If this value is positive, it sets the maximum value of mstar allowed in ePBL.
! (This is not used if EPBL_MSTAR_SCHEME = CONSTANT).
RH18_MSTAR_CN3 = -6.0 ! [nondim] default = -5.0
! MSTAR_N coefficient 3 (exponential decay coefficient). The value of -5.0 is
! given in RH18. Increasing this increases how quickly the value of MSTAR
! decreases as Hf/ust increases.
NSTAR = 0.06 ! [nondim] default = 0.2
! The portion of the buoyant potential energy imparted by surface fluxes that is
! available to drive entrainment at the base of mixed layer when that energy is
! positive.
MSTAR_CONV_ADJ = 0.66 ! [nondim] default = 0.0
! Coefficient used for reducing mstar during convection due to reduction of
! stable density gradient.
EPBL_TRANSITION_SCALE = 0.01 ! [nondim] default = 0.1
! A scale for the mixing length in the transition layer at the edge of the
! boundary layer as a fraction of the boundary layer thickness.
MIX_LEN_EXPONENT = 1.0 ! [nondim] default = 2.0
! The exponent applied to the ratio of the distance to the MLD and the MLD depth
! which determines the shape of the mixing length. This is only used if
! USE_MLD_ITERATION is True.
EPBL_VEL_SCALE_SCHEME = "REICHL_H18" ! default = "CUBE_ROOT_TKE"
! Selects the method for translating TKE into turbulent velocities. Valid values
! are:
! CUBE_ROOT_TKE - A constant times the cube root of remaining TKE.
! REICHL_H18 - Use the scheme based on a combination of w* and v* as
! documented in Reichl & Hallberg, 2018.
WSTAR_USTAR_COEF = 15.0 ! [nondim] default = 1.0
! A ratio relating the efficiency with which convectively released energy is
! converted to a turbulent velocity, relative to mechanically forced TKE. Making
! this larger increases the BL diffusivity
EPBL_VEL_SCALE_FACTOR = 0.5477 ! [nondim] default = 1.0
! An overall nondimensional scaling factor for wT. Making this larger increases
! the PBL diffusivity.
VSTAR_SURF_FAC = 1.8258 ! [nondim] default = 1.2
! The proportionality times ustar to set vstar at the surface.
USE_LA_LI2016 = True ! [Boolean] default = False
! A logical to use the Li et al. 2016 (submitted) formula to determine the
! Langmuir number.
EPBL_LANGMUIR_SCHEME = "ADDITIVE" ! default = "NONE"
! EPBL_LANGMUIR_SCHEME selects the method for including Langmuir turbulence.
! Valid values are:
! NONE - Do not do any extra mixing due to Langmuir turbulence
! RESCALE - Use a multiplicative rescaling of mstar to account for Langmuir
! turbulence
! ADDITIVE - Add a Langmuir turblence contribution to mstar to other
! contributions
LT_ENHANCE_COEF = 0.1056 ! [nondim] default = 0.447
! Coefficient for Langmuir enhancement of mstar
LT_ENHANCE_EXP = -1.0 ! [nondim] default = -1.33
! Exponent for Langmuir enhancementt of mstar
LT_MOD_LAC1 = 0.0 ! [nondim] default = -0.87
! Coefficient for modification of Langmuir number due to MLD approaching Ekman
! depth.
LT_MOD_LAC4 = 0.8 ! [nondim] default = 0.95
! Coefficient for modification of Langmuir number due to ratio of Ekman to
! stable Obukhov depth.
LT_MOD_LAC5 = 0.8 ! [nondim] default = 0.95
! Coefficient for modification of Langmuir number due to ratio of Ekman to
! unstable Obukhov depth.
! === module MOM_opacity ===
PEN_SW_SCALE = 10.0 ! [m] default = 0.0
! The vertical absorption e-folding depth of the penetrating shortwave
! radiation.
PEN_SW_FRAC = 0.42 ! [nondim] default = 0.0
! The fraction of the shortwave radiation that penetrates below the surface.
! === module MOM_tracer_advect ===
TRACER_ADVECTION_SCHEME = "PPM:H3" ! default = "PLM"
! The horizontal transport scheme for tracers:
! PLM - Piecewise Linear Method
! PPM:H3 - Piecewise Parabolic Method (Huyhn 3rd order)
! PPM - Piecewise Parabolic Method (Colella-Woodward)
! === module MOM_tracer_hor_diff ===
CHECK_DIFFUSIVE_CFL = True ! [Boolean] default = False
! If true, use enough iterations the diffusion to ensure that the diffusive
! equivalent of the CFL limit is not violated. If false, always use the greater
! of 1 or MAX_TR_DIFFUSION_CFL iteration.
! === module MOM_sum_output ===
CALCULATE_APE = False ! [Boolean] default = True
! If true, calculate the available potential energy of the interfaces. Setting
! this to false reduces the memory footprint of high-PE-count models
! dramatically.
MAXTRUNC = 100000 ! [truncations save_interval-1] default = 0
! The run will be stopped, and the day set to a very large value if the velocity
! is truncated more than MAXTRUNC times between energy saves. Set MAXTRUNC to 0
! to stop if there is any truncation of velocities.
ENERGYSAVEDAYS = 0.0416666666666667 ! [days] default = 1.0
! The interval in units of TIMEUNIT between saves of the energies of the run and
! other globally summed diagnostics.
! === module ocean_stochastics_init ===
! === module ocean_model_init ===
! === module MOM_surface_forcing ===
MAX_P_SURF = 0.0 ! [Pa] default = -1.0
! The maximum surface pressure that can be exerted by the atmosphere and
! floating sea-ice or ice shelves. This is needed because the FMS coupling
! structure does not limit the water that can be frozen out of the ocean and the
! ice-ocean heat fluxes are treated explicitly. No limit is applied if a
! negative value is used.
CD_TIDES = 0.0018 ! [nondim] default = 1.0E-04
! The drag coefficient that applies to the tides.
USE_RIGID_SEA_ICE = True ! [Boolean] default = False
! If true, sea-ice is rigid enough to exert a nonhydrostatic pressure that
! resist vertical motion.
SEA_ICE_RIGID_MASS = 100.0 ! [kg m-2] default = 1000.0
! The mass of sea-ice per unit area at which the sea-ice starts to exhibit
! rigidity
LA_DEPTH_RATIO = 0.2 ! [nondim] default = 0.04
! The depth (normalized by BLD) to average Stokes drift over in Langmuir number
! calculation, where La = sqrt(ust/Stokes).