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Prepare ESMG-configs for changes in defaults #17

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27 changes: 27 additions & 0 deletions ocean_only/Kelvin_wave/barotropic/MOM_input
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Original file line number Diff line number Diff line change
Expand Up @@ -132,6 +132,13 @@ ROTATION = "betaplane" ! default = "2omegasinlat"
! USER - call a user modified routine.
F_0 = 1.0E-04 ! [s-1] default = 0.0
! The reference value of the Coriolis parameter with the betaplane option.
OBC_PROJECTION_BUG = True ! [Boolean] default = True
! If false, use only interior ocean points at OBCs to specify several
! calculations at OBC points, and it avoids applying a land mask at the bay-like
! intersection of orthogonal OBC segments. Otherwise the calculation of terms
! like the potential vorticity used in the barotropic solver relies on
! bathymetry or other fields being projected outward across OBCs. This option
! changes answers for some configurations that use OBCs.

! === module MOM_verticalGrid ===
! Parameters providing information about the vertical grid.
Expand All @@ -147,6 +154,9 @@ USE_KELVIN_WAVE_OBC = True ! [Boolean] default = False
! If true, use the Kelvin wave open boundary.

! === module register_Kelvin_OBC ===
KELVIN_SET_OBC_INDEXING_BUGS = False ! [Boolean] default = True
! If true, retain several horizontal indexing bugs that were in the original
! version of Kelvin_set_OBC_data.

! === module MOM_coord_initialization ===
COORD_CONFIG = "linear" ! default = "none"
Expand Down Expand Up @@ -264,15 +274,32 @@ HMIX_FIXED = 20.0 ! [m]
! elevated when the bulk mixed layer is not used.

! === module MOM_barotropic ===
INTEGRAL_BT_CONTINUITY = False ! [Boolean] default = False
! If true, use the time-integrated velocity over the barotropic steps to
! determine the integrated transports used to update the continuity equation.
! Otherwise the transports are the sum of the transports based on a series of
! instantaneous velocities and the BT_CONT_TYPE for transports. This is only
! valid if USE_BT_CONT_TYPE = True.
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.
ADJUST_BT_CONT = False ! [Boolean] default = False
! If true, adjust the curve fit to the BT_cont type that is used by the
! barotropic solver to match the transport about which the flow is being
! linearized.
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 = False ! [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
! accelerations. Otherwise use the depth based on bathyT.
LINEARIZED_BT_CORIOLIS = True ! [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
Expand Down
17 changes: 17 additions & 0 deletions ocean_only/Tidal_bay/MOM_input
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Expand Up @@ -286,15 +286,32 @@ MAXVEL = 10.0 ! [m s-1] default = 3.0E+08
! The maximum velocity allowed before the velocity components are truncated.

! === module MOM_barotropic ===
INTEGRAL_BT_CONTINUITY = False ! [Boolean] default = False
! If true, use the time-integrated velocity over the barotropic steps to
! determine the integrated transports used to update the continuity equation.
! Otherwise the transports are the sum of the transports based on a series of
! instantaneous velocities and the BT_CONT_TYPE for transports. This is only
! valid if USE_BT_CONT_TYPE = True.
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.
ADJUST_BT_CONT = False ! [Boolean] default = False
! If true, adjust the curve fit to the BT_cont type that is used by the
! barotropic solver to match the transport about which the flow is being
! linearized.
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 = False ! [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
! accelerations. Otherwise use the depth based on bathyT.
LINEARIZED_BT_CORIOLIS = True ! [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
Expand Down
20 changes: 20 additions & 0 deletions ocean_only/channel/common/MOM_input
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Expand Up @@ -134,6 +134,9 @@ NUM_DYE_TRACERS = 1 ! default = 0
! === module MOM_boundary_update ===
USE_DYED_CHANNEL_OBC = True ! [Boolean] default = False
! If true, use the dyed channel open boundary.
CHANNEL_FLOW_OBC_TRANSPORT_BUG = False ! [Boolean] default = True
! If true and specified open boundary conditions are being used, use a 1 m (if
! Boussienesq) or 1 kg m-2 layer thickness instead of the actual thickness.

! === module MOM_coord_initialization ===
COORD_CONFIG = "linear" ! default = "none"
Expand Down Expand Up @@ -272,15 +275,32 @@ HMIX_FIXED = 20.0 ! [m]
! elevated when the bulk mixed layer is not used.

! === module MOM_barotropic ===
INTEGRAL_BT_CONTINUITY = False ! [Boolean] default = False
! If true, use the time-integrated velocity over the barotropic steps to
! determine the integrated transports used to update the continuity equation.
! Otherwise the transports are the sum of the transports based on a series of
! instantaneous velocities and the BT_CONT_TYPE for transports. This is only
! valid if USE_BT_CONT_TYPE = True.
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.
ADJUST_BT_CONT = False ! [Boolean] default = False
! If true, adjust the curve fit to the BT_cont type that is used by the
! barotropic solver to match the transport about which the flow is being
! linearized.
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 = False ! [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
! accelerations. Otherwise use the depth based on bathyT.
LINEARIZED_BT_CORIOLIS = True ! [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
Expand Down
24 changes: 24 additions & 0 deletions ocean_only/shelfwave/MOM_input
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Original file line number Diff line number Diff line change
Expand Up @@ -119,6 +119,13 @@ ROTATION = "betaplane" ! default = "2omegasinlat"
! USER - call a user modified routine.
F_0 = 1.0E-04 ! [s-1] default = 0.0
! The reference value of the Coriolis parameter with the betaplane option.
OBC_PROJECTION_BUG = True ! [Boolean] default = True
! If false, use only interior ocean points at OBCs to specify several
! calculations at OBC points, and it avoids applying a land mask at the bay-like
! intersection of orthogonal OBC segments. Otherwise the calculation of terms
! like the potential vorticity used in the barotropic solver relies on
! bathymetry or other fields being projected outward across OBCs. This option
! changes answers for some configurations that use OBCs.

! === module MOM_verticalGrid ===
! Parameters providing information about the vertical grid.
Expand Down Expand Up @@ -251,15 +258,32 @@ HMIX_FIXED = 20.0 ! [m]
! elevated when the bulk mixed layer is not used.

! === module MOM_barotropic ===
INTEGRAL_BT_CONTINUITY = False ! [Boolean] default = False
! If true, use the time-integrated velocity over the barotropic steps to
! determine the integrated transports used to update the continuity equation.
! Otherwise the transports are the sum of the transports based on a series of
! instantaneous velocities and the BT_CONT_TYPE for transports. This is only
! valid if USE_BT_CONT_TYPE = True.
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.
ADJUST_BT_CONT = False ! [Boolean] default = False
! If true, adjust the curve fit to the BT_cont type that is used by the
! barotropic solver to match the transport about which the flow is being
! linearized.
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 = False ! [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
! accelerations. Otherwise use the depth based on bathyT.
LINEARIZED_BT_CORIOLIS = True ! [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
Expand Down