diff --git a/coupled_AM2_LM3_SIS2/AM2_SIS2_MOM6i_1deg/MOM_parameter_doc.all b/coupled_AM2_LM3_SIS2/AM2_SIS2_MOM6i_1deg/MOM_parameter_doc.all index b022159bd..b7848fc64 100644 --- a/coupled_AM2_LM3_SIS2/AM2_SIS2_MOM6i_1deg/MOM_parameter_doc.all +++ b/coupled_AM2_LM3_SIS2/AM2_SIS2_MOM6i_1deg/MOM_parameter_doc.all @@ -710,12 +710,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.25 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -732,6 +750,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_SIMPLER_EADY_GROWTH_RATE = False ! [Boolean] default = False ! If true, use a simpler method to calculate the Eady growth rate that avoids ! division by layer thickness. Recommended. @@ -912,9 +933,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1979,9 +1997,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 10.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 50.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 900.0 ! [m2 s-1] default = 0.0 diff --git a/coupled_AM2_LM3_SIS2/Concurrent_ice_1deg/MOM_parameter_doc.all b/coupled_AM2_LM3_SIS2/Concurrent_ice_1deg/MOM_parameter_doc.all index 17876f947..eedfdb4d6 100644 --- a/coupled_AM2_LM3_SIS2/Concurrent_ice_1deg/MOM_parameter_doc.all +++ b/coupled_AM2_LM3_SIS2/Concurrent_ice_1deg/MOM_parameter_doc.all @@ -710,12 +710,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.25 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -732,6 +750,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_SIMPLER_EADY_GROWTH_RATE = False ! [Boolean] default = False ! If true, use a simpler method to calculate the Eady growth rate that avoids ! division by layer thickness. Recommended. @@ -912,9 +933,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1979,9 +1997,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 10.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 50.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 900.0 ! [m2 s-1] default = 0.0 diff --git a/coupled_AM2_LM3_SIS2/Intersperse_ice_1deg/MOM_parameter_doc.all b/coupled_AM2_LM3_SIS2/Intersperse_ice_1deg/MOM_parameter_doc.all index e7285bcf5..bd1074c53 100644 --- a/coupled_AM2_LM3_SIS2/Intersperse_ice_1deg/MOM_parameter_doc.all +++ b/coupled_AM2_LM3_SIS2/Intersperse_ice_1deg/MOM_parameter_doc.all @@ -710,12 +710,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.25 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -732,6 +750,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_SIMPLER_EADY_GROWTH_RATE = False ! [Boolean] default = False ! If true, use a simpler method to calculate the Eady growth rate that avoids ! division by layer thickness. Recommended. @@ -912,9 +933,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1979,9 +1997,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 10.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 50.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 900.0 ! [m2 s-1] default = 0.0 diff --git a/ice_ocean_SIS2/Baltic/MOM_parameter_doc.all b/ice_ocean_SIS2/Baltic/MOM_parameter_doc.all index 2f870b864..cdab5f4c8 100644 --- a/ice_ocean_SIS2/Baltic/MOM_parameter_doc.all +++ b/ice_ocean_SIS2/Baltic/MOM_parameter_doc.all @@ -710,12 +710,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.25 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -732,6 +750,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_SIMPLER_EADY_GROWTH_RATE = False ! [Boolean] default = False ! If true, use a simpler method to calculate the Eady growth rate that avoids ! division by layer thickness. Recommended. @@ -912,9 +933,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1979,9 +1997,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 10.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 50.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 900.0 ! [m2 s-1] default = 0.0 diff --git a/ice_ocean_SIS2/Baltic_ALE_z_offline_tracers/MOM_parameter_doc.all b/ice_ocean_SIS2/Baltic_ALE_z_offline_tracers/MOM_parameter_doc.all index 25d38516e..79d541c38 100644 --- a/ice_ocean_SIS2/Baltic_ALE_z_offline_tracers/MOM_parameter_doc.all +++ b/ice_ocean_SIS2/Baltic_ALE_z_offline_tracers/MOM_parameter_doc.all @@ -860,6 +860,8 @@ MEKE_TOPOGRAPHIC_BETA = 0.0 ! [nondim] default = 0.0 ! A scale factor to determine how much topographic beta is weighed in computing ! beta in the expression of Rhines scale. Use 1 if full topographic beta effect ! is considered; use 0 if it's completely ignored. +SQG_USE_MEKE = False ! [Boolean] default = False + ! If true, the eddy scale of MEKE is used for the SQG vertical structure CDRAG = 0.003 ! [nondim] default = 0.003 ! CDRAG is the drag coefficient relating the magnitude of the velocity field to ! the bottom stress. @@ -896,12 +898,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -2219,9 +2239,6 @@ USE_HUYNH_STENCIL_BUG = False ! [Boolean] default = False ! === module MOM_tracer_hor_diff === KHTR = 600.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 50.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 900.0 ! [m2 s-1] default = 0.0 diff --git a/ice_ocean_SIS2/Baltic_OM4_025/MOM_parameter_doc.all b/ice_ocean_SIS2/Baltic_OM4_025/MOM_parameter_doc.all index 759cd9e3a..91b169908 100644 --- a/ice_ocean_SIS2/Baltic_OM4_025/MOM_parameter_doc.all +++ b/ice_ocean_SIS2/Baltic_OM4_025/MOM_parameter_doc.all @@ -949,6 +949,8 @@ MEKE_TOPOGRAPHIC_BETA = 0.0 ! [nondim] default = 0.0 ! A scale factor to determine how much topographic beta is weighed in computing ! beta in the expression of Rhines scale. Use 1 if full topographic beta effect ! is considered; use 0 if it's completely ignored. +SQG_USE_MEKE = False ! [Boolean] default = False + ! If true, the eddy scale of MEKE is used for the SQG vertical structure CDRAG = 0.003 ! [nondim] default = 0.003 ! CDRAG is the drag coefficient relating the magnitude of the velocity field to ! the bottom stress. @@ -985,12 +987,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -2297,9 +2317,6 @@ USE_HUYNH_STENCIL_BUG = False ! [Boolean] default = False ! === module MOM_tracer_hor_diff === KHTR = 0.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ice_ocean_SIS2/Baltic_OM4_05/MOM_parameter_doc.all b/ice_ocean_SIS2/Baltic_OM4_05/MOM_parameter_doc.all index 2fa75afd2..e0c63b8f2 100644 --- a/ice_ocean_SIS2/Baltic_OM4_05/MOM_parameter_doc.all +++ b/ice_ocean_SIS2/Baltic_OM4_05/MOM_parameter_doc.all @@ -949,6 +949,8 @@ MEKE_TOPOGRAPHIC_BETA = 0.0 ! [nondim] default = 0.0 ! A scale factor to determine how much topographic beta is weighed in computing ! beta in the expression of Rhines scale. Use 1 if full topographic beta effect ! is considered; use 0 if it's completely ignored. +SQG_USE_MEKE = False ! [Boolean] default = False + ! If true, the eddy scale of MEKE is used for the SQG vertical structure CDRAG = 0.003 ! [nondim] default = 0.003 ! CDRAG is the drag coefficient relating the magnitude of the velocity field to ! the bottom stress. @@ -985,12 +987,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = True ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -2316,9 +2336,6 @@ USE_HUYNH_STENCIL_BUG = False ! [Boolean] default = False ! === module MOM_tracer_hor_diff === KHTR = 50.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ice_ocean_SIS2/OM4_025/MOM_parameter_doc.all b/ice_ocean_SIS2/OM4_025/MOM_parameter_doc.all index c9cfbe1bf..c8e2c4dbe 100644 --- a/ice_ocean_SIS2/OM4_025/MOM_parameter_doc.all +++ b/ice_ocean_SIS2/OM4_025/MOM_parameter_doc.all @@ -949,6 +949,8 @@ MEKE_TOPOGRAPHIC_BETA = 0.0 ! [nondim] default = 0.0 ! A scale factor to determine how much topographic beta is weighed in computing ! beta in the expression of Rhines scale. Use 1 if full topographic beta effect ! is considered; use 0 if it's completely ignored. +SQG_USE_MEKE = False ! [Boolean] default = False + ! If true, the eddy scale of MEKE is used for the SQG vertical structure CDRAG = 0.003 ! [nondim] default = 0.003 ! CDRAG is the drag coefficient relating the magnitude of the velocity field to ! the bottom stress. @@ -985,12 +987,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -2297,9 +2317,6 @@ USE_HUYNH_STENCIL_BUG = False ! [Boolean] default = False ! === module MOM_tracer_hor_diff === KHTR = 0.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ice_ocean_SIS2/OM4_05/MOM_parameter_doc.all b/ice_ocean_SIS2/OM4_05/MOM_parameter_doc.all index 774322c0c..9c6094534 100644 --- a/ice_ocean_SIS2/OM4_05/MOM_parameter_doc.all +++ b/ice_ocean_SIS2/OM4_05/MOM_parameter_doc.all @@ -949,6 +949,8 @@ MEKE_TOPOGRAPHIC_BETA = 0.0 ! [nondim] default = 0.0 ! A scale factor to determine how much topographic beta is weighed in computing ! beta in the expression of Rhines scale. Use 1 if full topographic beta effect ! is considered; use 0 if it's completely ignored. +SQG_USE_MEKE = False ! [Boolean] default = False + ! If true, the eddy scale of MEKE is used for the SQG vertical structure CDRAG = 0.003 ! [nondim] default = 0.003 ! CDRAG is the drag coefficient relating the magnitude of the velocity field to ! the bottom stress. @@ -985,12 +987,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = True ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -2316,9 +2336,6 @@ USE_HUYNH_STENCIL_BUG = False ! [Boolean] default = False ! === module MOM_tracer_hor_diff === KHTR = 50.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ice_ocean_SIS2/OM_1deg/MOM_parameter_doc.all b/ice_ocean_SIS2/OM_1deg/MOM_parameter_doc.all index bbfec6ec9..867e964de 100644 --- a/ice_ocean_SIS2/OM_1deg/MOM_parameter_doc.all +++ b/ice_ocean_SIS2/OM_1deg/MOM_parameter_doc.all @@ -940,6 +940,8 @@ MEKE_TOPOGRAPHIC_BETA = 0.0 ! [nondim] default = 0.0 ! A scale factor to determine how much topographic beta is weighed in computing ! beta in the expression of Rhines scale. Use 1 if full topographic beta effect ! is considered; use 0 if it's completely ignored. +SQG_USE_MEKE = False ! [Boolean] default = False + ! If true, the eddy scale of MEKE is used for the SQG vertical structure CDRAG = 0.003 ! [nondim] default = 0.003 ! CDRAG is the drag coefficient relating the magnitude of the velocity field to ! the bottom stress. @@ -976,12 +978,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -2259,9 +2279,6 @@ USE_HUYNH_STENCIL_BUG = False ! [Boolean] default = False ! === module MOM_tracer_hor_diff === KHTR = 0.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ice_ocean_SIS2/SIS2/MOM_parameter_doc.all b/ice_ocean_SIS2/SIS2/MOM_parameter_doc.all index 253dd63a4..0667b405f 100644 --- a/ice_ocean_SIS2/SIS2/MOM_parameter_doc.all +++ b/ice_ocean_SIS2/SIS2/MOM_parameter_doc.all @@ -676,12 +676,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.25 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -698,6 +716,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_SIMPLER_EADY_GROWTH_RATE = False ! [Boolean] default = False ! If true, use a simpler method to calculate the Eady growth rate that avoids ! division by layer thickness. Recommended. @@ -878,9 +899,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1945,9 +1963,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 10.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 50.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 900.0 ! [m2 s-1] default = 0.0 diff --git a/ice_ocean_SIS2/SIS2_bergs_cgrid/MOM_parameter_doc.all b/ice_ocean_SIS2/SIS2_bergs_cgrid/MOM_parameter_doc.all index 04df58801..7cea443d5 100644 --- a/ice_ocean_SIS2/SIS2_bergs_cgrid/MOM_parameter_doc.all +++ b/ice_ocean_SIS2/SIS2_bergs_cgrid/MOM_parameter_doc.all @@ -676,12 +676,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.25 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -698,6 +716,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_SIMPLER_EADY_GROWTH_RATE = False ! [Boolean] default = False ! If true, use a simpler method to calculate the Eady growth rate that avoids ! division by layer thickness. Recommended. @@ -878,9 +899,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1949,9 +1967,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 10.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 50.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 900.0 ! [m2 s-1] default = 0.0 diff --git a/ice_ocean_SIS2/SIS2_cgrid/MOM_parameter_doc.all b/ice_ocean_SIS2/SIS2_cgrid/MOM_parameter_doc.all index d5e422cc2..01732242b 100644 --- a/ice_ocean_SIS2/SIS2_cgrid/MOM_parameter_doc.all +++ b/ice_ocean_SIS2/SIS2_cgrid/MOM_parameter_doc.all @@ -676,12 +676,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.25 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -698,6 +716,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_SIMPLER_EADY_GROWTH_RATE = False ! [Boolean] default = False ! If true, use a simpler method to calculate the Eady growth rate that avoids ! division by layer thickness. Recommended. @@ -878,9 +899,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1945,9 +1963,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 10.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 50.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 900.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/CVmix_SCM_tests/cooling_only/BML/MOM_parameter_doc.all b/ocean_only/CVmix_SCM_tests/cooling_only/BML/MOM_parameter_doc.all index c36b4ff80..66ee4dacb 100644 --- a/ocean_only/CVmix_SCM_tests/cooling_only/BML/MOM_parameter_doc.all +++ b/ocean_only/CVmix_SCM_tests/cooling_only/BML/MOM_parameter_doc.all @@ -582,12 +582,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -604,6 +622,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -707,9 +728,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1351,9 +1369,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 600.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/CVmix_SCM_tests/cooling_only/EPBL/MOM_parameter_doc.all b/ocean_only/CVmix_SCM_tests/cooling_only/EPBL/MOM_parameter_doc.all index 99079cc63..b44ce0220 100644 --- a/ocean_only/CVmix_SCM_tests/cooling_only/EPBL/MOM_parameter_doc.all +++ b/ocean_only/CVmix_SCM_tests/cooling_only/EPBL/MOM_parameter_doc.all @@ -701,12 +701,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -723,6 +741,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -826,9 +847,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1465,9 +1483,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 600.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/CVmix_SCM_tests/cooling_only/KPP/MOM_parameter_doc.all b/ocean_only/CVmix_SCM_tests/cooling_only/KPP/MOM_parameter_doc.all index fa4305a3b..8ddcdf511 100644 --- a/ocean_only/CVmix_SCM_tests/cooling_only/KPP/MOM_parameter_doc.all +++ b/ocean_only/CVmix_SCM_tests/cooling_only/KPP/MOM_parameter_doc.all @@ -701,12 +701,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -723,6 +741,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -826,9 +847,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1465,9 +1483,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 600.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/CVmix_SCM_tests/mech_only/BML/MOM_parameter_doc.all b/ocean_only/CVmix_SCM_tests/mech_only/BML/MOM_parameter_doc.all index 5a9b1cfe0..44ec9ba1c 100644 --- a/ocean_only/CVmix_SCM_tests/mech_only/BML/MOM_parameter_doc.all +++ b/ocean_only/CVmix_SCM_tests/mech_only/BML/MOM_parameter_doc.all @@ -582,12 +582,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -604,6 +622,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -707,9 +728,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1351,9 +1369,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 600.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/CVmix_SCM_tests/mech_only/EPBL/MOM_parameter_doc.all b/ocean_only/CVmix_SCM_tests/mech_only/EPBL/MOM_parameter_doc.all index 3e5a9a148..63ed62265 100644 --- a/ocean_only/CVmix_SCM_tests/mech_only/EPBL/MOM_parameter_doc.all +++ b/ocean_only/CVmix_SCM_tests/mech_only/EPBL/MOM_parameter_doc.all @@ -701,12 +701,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -723,6 +741,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -826,9 +847,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1465,9 +1483,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 600.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/CVmix_SCM_tests/mech_only/KPP/MOM_parameter_doc.all b/ocean_only/CVmix_SCM_tests/mech_only/KPP/MOM_parameter_doc.all index d06728e7d..adcaf759e 100644 --- a/ocean_only/CVmix_SCM_tests/mech_only/KPP/MOM_parameter_doc.all +++ b/ocean_only/CVmix_SCM_tests/mech_only/KPP/MOM_parameter_doc.all @@ -701,12 +701,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -723,6 +741,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -826,9 +847,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1465,9 +1483,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 600.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/CVmix_SCM_tests/skin_warming_wind/BML/MOM_parameter_doc.all b/ocean_only/CVmix_SCM_tests/skin_warming_wind/BML/MOM_parameter_doc.all index 992e23fb5..ba7e8d03c 100644 --- a/ocean_only/CVmix_SCM_tests/skin_warming_wind/BML/MOM_parameter_doc.all +++ b/ocean_only/CVmix_SCM_tests/skin_warming_wind/BML/MOM_parameter_doc.all @@ -582,12 +582,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -604,6 +622,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -707,9 +728,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1351,9 +1369,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 600.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/CVmix_SCM_tests/skin_warming_wind/EPBL/MOM_parameter_doc.all b/ocean_only/CVmix_SCM_tests/skin_warming_wind/EPBL/MOM_parameter_doc.all index 83d0692ca..3e93c4c80 100644 --- a/ocean_only/CVmix_SCM_tests/skin_warming_wind/EPBL/MOM_parameter_doc.all +++ b/ocean_only/CVmix_SCM_tests/skin_warming_wind/EPBL/MOM_parameter_doc.all @@ -701,12 +701,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -723,6 +741,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -826,9 +847,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1465,9 +1483,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 600.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/CVmix_SCM_tests/skin_warming_wind/KPP/MOM_parameter_doc.all b/ocean_only/CVmix_SCM_tests/skin_warming_wind/KPP/MOM_parameter_doc.all index 1e9fd1b62..ca09737d7 100644 --- a/ocean_only/CVmix_SCM_tests/skin_warming_wind/KPP/MOM_parameter_doc.all +++ b/ocean_only/CVmix_SCM_tests/skin_warming_wind/KPP/MOM_parameter_doc.all @@ -701,12 +701,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -723,6 +741,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -826,9 +847,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1465,9 +1483,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 600.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/CVmix_SCM_tests/wind_only/BML/MOM_parameter_doc.all b/ocean_only/CVmix_SCM_tests/wind_only/BML/MOM_parameter_doc.all index 65cdb676c..8963856d8 100644 --- a/ocean_only/CVmix_SCM_tests/wind_only/BML/MOM_parameter_doc.all +++ b/ocean_only/CVmix_SCM_tests/wind_only/BML/MOM_parameter_doc.all @@ -582,12 +582,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -604,6 +622,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -707,9 +728,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1351,9 +1369,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 600.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/CVmix_SCM_tests/wind_only/EPBL/MOM_parameter_doc.all b/ocean_only/CVmix_SCM_tests/wind_only/EPBL/MOM_parameter_doc.all index 97e4fa565..b30067bf3 100644 --- a/ocean_only/CVmix_SCM_tests/wind_only/EPBL/MOM_parameter_doc.all +++ b/ocean_only/CVmix_SCM_tests/wind_only/EPBL/MOM_parameter_doc.all @@ -701,12 +701,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -723,6 +741,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -826,9 +847,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1465,9 +1483,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 600.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/CVmix_SCM_tests/wind_only/KPP/MOM_parameter_doc.all b/ocean_only/CVmix_SCM_tests/wind_only/KPP/MOM_parameter_doc.all index 3c454642e..5a25851eb 100644 --- a/ocean_only/CVmix_SCM_tests/wind_only/KPP/MOM_parameter_doc.all +++ b/ocean_only/CVmix_SCM_tests/wind_only/KPP/MOM_parameter_doc.all @@ -701,12 +701,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -723,6 +741,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -826,9 +847,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1465,9 +1483,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 600.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/DOME/MOM_parameter_doc.all b/ocean_only/DOME/MOM_parameter_doc.all index b4359ca94..9c26834fc 100644 --- a/ocean_only/DOME/MOM_parameter_doc.all +++ b/ocean_only/DOME/MOM_parameter_doc.all @@ -641,12 +641,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -663,6 +681,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -762,9 +783,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1469,9 +1487,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 0.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/Phillips_2layer/MOM_parameter_doc.all b/ocean_only/Phillips_2layer/MOM_parameter_doc.all index 8558e0af7..bf6af1637 100644 --- a/ocean_only/Phillips_2layer/MOM_parameter_doc.all +++ b/ocean_only/Phillips_2layer/MOM_parameter_doc.all @@ -530,12 +530,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -552,6 +570,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. KH_RES_SCALE_COEF = 0.707106781 ! [nondim] default = 1.0 ! A coefficient that determines how KhTh is scaled away if RESOLN_SCALED_... is ! true, as F = 1 / (1 + (KH_RES_SCALE_COEF*Rd/dx)^KH_RES_FN_POWER). @@ -687,9 +708,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1324,9 +1342,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 0.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/SCM_idealized_hurricane/MOM_parameter_doc.all b/ocean_only/SCM_idealized_hurricane/MOM_parameter_doc.all index d37891c10..7353172c0 100644 --- a/ocean_only/SCM_idealized_hurricane/MOM_parameter_doc.all +++ b/ocean_only/SCM_idealized_hurricane/MOM_parameter_doc.all @@ -701,12 +701,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -723,6 +741,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -826,9 +847,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1465,9 +1483,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 600.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/adjustment2d/layer/MOM_parameter_doc.all b/ocean_only/adjustment2d/layer/MOM_parameter_doc.all index 3ca227abf..309245a1e 100644 --- a/ocean_only/adjustment2d/layer/MOM_parameter_doc.all +++ b/ocean_only/adjustment2d/layer/MOM_parameter_doc.all @@ -604,12 +604,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -626,6 +644,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -729,9 +750,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1468,9 +1486,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 0.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/adjustment2d/rho/MOM_parameter_doc.all b/ocean_only/adjustment2d/rho/MOM_parameter_doc.all index 8cd1051c4..977248a27 100644 --- a/ocean_only/adjustment2d/rho/MOM_parameter_doc.all +++ b/ocean_only/adjustment2d/rho/MOM_parameter_doc.all @@ -768,12 +768,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -790,6 +808,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -893,9 +914,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1628,9 +1646,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 0.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/adjustment2d/z/MOM_parameter_doc.all b/ocean_only/adjustment2d/z/MOM_parameter_doc.all index 2f99b2167..09e497acc 100644 --- a/ocean_only/adjustment2d/z/MOM_parameter_doc.all +++ b/ocean_only/adjustment2d/z/MOM_parameter_doc.all @@ -720,12 +720,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -742,6 +760,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -845,9 +866,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1580,9 +1598,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 0.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/benchmark/MOM_parameter_doc.all b/ocean_only/benchmark/MOM_parameter_doc.all index bafe0167d..95283ccfc 100644 --- a/ocean_only/benchmark/MOM_parameter_doc.all +++ b/ocean_only/benchmark/MOM_parameter_doc.all @@ -633,12 +633,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.1 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -655,6 +673,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_SIMPLER_EADY_GROWTH_RATE = False ! [Boolean] default = False ! If true, use a simpler method to calculate the Eady growth rate that avoids ! division by layer thickness. Recommended. @@ -822,9 +843,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1729,9 +1747,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 1.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 900.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/circle_obcs/MOM_parameter_doc.all b/ocean_only/circle_obcs/MOM_parameter_doc.all index 53d72bcf7..2bda90678 100644 --- a/ocean_only/circle_obcs/MOM_parameter_doc.all +++ b/ocean_only/circle_obcs/MOM_parameter_doc.all @@ -639,12 +639,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -661,6 +679,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -760,9 +781,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1546,9 +1564,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 0.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/double_gyre/MOM_parameter_doc.all b/ocean_only/double_gyre/MOM_parameter_doc.all index d7fea311d..3a6f39021 100644 --- a/ocean_only/double_gyre/MOM_parameter_doc.all +++ b/ocean_only/double_gyre/MOM_parameter_doc.all @@ -497,12 +497,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -519,6 +537,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -616,9 +637,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1086,9 +1104,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 0.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/external_gwave/MOM_parameter_doc.all b/ocean_only/external_gwave/MOM_parameter_doc.all index e923362a9..53a944b3b 100644 --- a/ocean_only/external_gwave/MOM_parameter_doc.all +++ b/ocean_only/external_gwave/MOM_parameter_doc.all @@ -593,12 +593,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -615,6 +633,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -718,9 +739,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1454,9 +1472,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 0.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/flow_downslope/layer/MOM_parameter_doc.all b/ocean_only/flow_downslope/layer/MOM_parameter_doc.all index 20d46a9db..243ee18bd 100644 --- a/ocean_only/flow_downslope/layer/MOM_parameter_doc.all +++ b/ocean_only/flow_downslope/layer/MOM_parameter_doc.all @@ -603,12 +603,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -625,6 +643,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -728,9 +749,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1465,9 +1483,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 0.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/flow_downslope/rho/MOM_parameter_doc.all b/ocean_only/flow_downslope/rho/MOM_parameter_doc.all index 028c7d364..71f3e0783 100644 --- a/ocean_only/flow_downslope/rho/MOM_parameter_doc.all +++ b/ocean_only/flow_downslope/rho/MOM_parameter_doc.all @@ -769,12 +769,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -791,6 +809,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -894,9 +915,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1627,9 +1645,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 0.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/flow_downslope/sigma/MOM_parameter_doc.all b/ocean_only/flow_downslope/sigma/MOM_parameter_doc.all index 906dbcf17..443160903 100644 --- a/ocean_only/flow_downslope/sigma/MOM_parameter_doc.all +++ b/ocean_only/flow_downslope/sigma/MOM_parameter_doc.all @@ -721,12 +721,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -743,6 +761,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -846,9 +867,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1579,9 +1597,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 0.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/flow_downslope/z/MOM_parameter_doc.all b/ocean_only/flow_downslope/z/MOM_parameter_doc.all index bc7b83031..700a44c41 100644 --- a/ocean_only/flow_downslope/z/MOM_parameter_doc.all +++ b/ocean_only/flow_downslope/z/MOM_parameter_doc.all @@ -721,12 +721,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -743,6 +761,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -846,9 +867,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1579,9 +1597,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 0.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/global_ALE/hycom/MOM_parameter_doc.all b/ocean_only/global_ALE/hycom/MOM_parameter_doc.all index c124e0f6b..714fe0bee 100644 --- a/ocean_only/global_ALE/hycom/MOM_parameter_doc.all +++ b/ocean_only/global_ALE/hycom/MOM_parameter_doc.all @@ -900,6 +900,8 @@ MEKE_TOPOGRAPHIC_BETA = 0.0 ! [nondim] default = 0.0 ! A scale factor to determine how much topographic beta is weighed in computing ! beta in the expression of Rhines scale. Use 1 if full topographic beta effect ! is considered; use 0 if it's completely ignored. +SQG_USE_MEKE = False ! [Boolean] default = False + ! If true, the eddy scale of MEKE is used for the SQG vertical structure CDRAG = 0.003 ! [nondim] default = 0.003 ! CDRAG is the drag coefficient relating the magnitude of the velocity field to ! the bottom stress. @@ -936,12 +938,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -2272,9 +2292,6 @@ USE_HUYNH_STENCIL_BUG = False ! [Boolean] default = False ! === module MOM_tracer_hor_diff === KHTR = 600.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 50.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 900.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/global_ALE/layer/MOM_parameter_doc.all b/ocean_only/global_ALE/layer/MOM_parameter_doc.all index 01f938041..e1b3d2b97 100644 --- a/ocean_only/global_ALE/layer/MOM_parameter_doc.all +++ b/ocean_only/global_ALE/layer/MOM_parameter_doc.all @@ -775,6 +775,8 @@ MEKE_TOPOGRAPHIC_BETA = 0.0 ! [nondim] default = 0.0 ! A scale factor to determine how much topographic beta is weighed in computing ! beta in the expression of Rhines scale. Use 1 if full topographic beta effect ! is considered; use 0 if it's completely ignored. +SQG_USE_MEKE = False ! [Boolean] default = False + ! If true, the eddy scale of MEKE is used for the SQG vertical structure CDRAG = 0.003 ! [nondim] default = 0.003 ! CDRAG is the drag coefficient relating the magnitude of the velocity field to ! the bottom stress. @@ -811,12 +813,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -833,6 +853,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_SIMPLER_EADY_GROWTH_RATE = False ! [Boolean] default = False ! If true, use a simpler method to calculate the Eady growth rate that avoids ! division by layer thickness. Recommended. @@ -995,9 +1018,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = True ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -2144,9 +2164,6 @@ USE_HUYNH_STENCIL_BUG = False ! [Boolean] default = False ! === module MOM_tracer_hor_diff === KHTR = 600.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 50.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 900.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/global_ALE/layer/available_diags.000000 b/ocean_only/global_ALE/layer/available_diags.000000 index 05493443b..84ad9fe85 100644 --- a/ocean_only/global_ALE/layer/available_diags.000000 +++ b/ocean_only/global_ALE/layer/available_diags.000000 @@ -268,6 +268,12 @@ ! long_name: Inverse eddy time-scale, S*N, at v-points ! units: s-1 ! cell_methods: xh:mean yq:point +"sqg_struct" [Unused] + ! modules: {ocean_model,ocean_model_z,ocean_model_d2,ocean_model_z_d2} + ! long_name: Vertical structure of SQG mode + ! units: nondim + ! cell_methods: xh:mean yh:mean zl:mean area:mean + ! variants: {sqg_struct,sqg_struct_xyave} "Res_fn" [Unused] ! modules: {ocean_model,ocean_model_d2} ! long_name: Resolution function for scaling diffusivities diff --git a/ocean_only/global_ALE/z/MOM_parameter_doc.all b/ocean_only/global_ALE/z/MOM_parameter_doc.all index 7b3365ab3..a915a9dab 100644 --- a/ocean_only/global_ALE/z/MOM_parameter_doc.all +++ b/ocean_only/global_ALE/z/MOM_parameter_doc.all @@ -847,6 +847,8 @@ MEKE_TOPOGRAPHIC_BETA = 0.0 ! [nondim] default = 0.0 ! A scale factor to determine how much topographic beta is weighed in computing ! beta in the expression of Rhines scale. Use 1 if full topographic beta effect ! is considered; use 0 if it's completely ignored. +SQG_USE_MEKE = False ! [Boolean] default = False + ! If true, the eddy scale of MEKE is used for the SQG vertical structure CDRAG = 0.003 ! [nondim] default = 0.003 ! CDRAG is the drag coefficient relating the magnitude of the velocity field to ! the bottom stress. @@ -883,12 +885,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -2219,9 +2239,6 @@ USE_HUYNH_STENCIL_BUG = False ! [Boolean] default = False ! === module MOM_tracer_hor_diff === KHTR = 600.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 50.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 900.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/global_ALE/z/available_diags.000000 b/ocean_only/global_ALE/z/available_diags.000000 index 805798007..bb0ca8688 100644 --- a/ocean_only/global_ALE/z/available_diags.000000 +++ b/ocean_only/global_ALE/z/available_diags.000000 @@ -268,6 +268,12 @@ ! long_name: Inverse eddy time-scale, S*N, at v-points ! units: s-1 ! cell_methods: xh:mean yq:point +"sqg_struct" [Unused] + ! modules: {ocean_model,ocean_model_z,ocean_model_d2,ocean_model_z_d2} + ! long_name: Vertical structure of SQG mode + ! units: nondim + ! cell_methods: xh:mean yh:mean zl:mean area:mean + ! variants: {sqg_struct,sqg_struct_xyave} "N2_u" [Unused] ! modules: {ocean_model,ocean_model_z,ocean_model_d2,ocean_model_z_d2} ! long_name: Square of Brunt-Vaisala frequency, N^2, at u-points, as used in Visbeck et al. diff --git a/ocean_only/lock_exchange/MOM_parameter_doc.all b/ocean_only/lock_exchange/MOM_parameter_doc.all index 19061684f..fe19229dd 100644 --- a/ocean_only/lock_exchange/MOM_parameter_doc.all +++ b/ocean_only/lock_exchange/MOM_parameter_doc.all @@ -596,12 +596,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -618,6 +636,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -721,9 +742,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1457,9 +1475,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 0.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/mixed_layer_restrat_2d/MOM_parameter_doc.all b/ocean_only/mixed_layer_restrat_2d/MOM_parameter_doc.all index a27c6dee3..bab751926 100644 --- a/ocean_only/mixed_layer_restrat_2d/MOM_parameter_doc.all +++ b/ocean_only/mixed_layer_restrat_2d/MOM_parameter_doc.all @@ -706,12 +706,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -728,6 +746,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -831,9 +852,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1617,9 +1635,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 0.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/nonBous_global/MOM_parameter_doc.all b/ocean_only/nonBous_global/MOM_parameter_doc.all index da3824a69..a71aba034 100644 --- a/ocean_only/nonBous_global/MOM_parameter_doc.all +++ b/ocean_only/nonBous_global/MOM_parameter_doc.all @@ -632,12 +632,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.25 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -654,6 +672,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_SIMPLER_EADY_GROWTH_RATE = False ! [Boolean] default = False ! If true, use a simpler method to calculate the Eady growth rate that avoids ! division by layer thickness. Recommended. @@ -830,9 +851,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1940,9 +1958,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 10.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 50.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 900.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/resting/layer/MOM_parameter_doc.all b/ocean_only/resting/layer/MOM_parameter_doc.all index 22f7d2fa2..62e9d8d91 100644 --- a/ocean_only/resting/layer/MOM_parameter_doc.all +++ b/ocean_only/resting/layer/MOM_parameter_doc.all @@ -588,12 +588,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -610,6 +628,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -713,9 +734,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1450,9 +1468,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 0.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/resting/z/MOM_parameter_doc.all b/ocean_only/resting/z/MOM_parameter_doc.all index f3c62047b..f69ec13b2 100644 --- a/ocean_only/resting/z/MOM_parameter_doc.all +++ b/ocean_only/resting/z/MOM_parameter_doc.all @@ -706,12 +706,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -728,6 +746,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -831,9 +852,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1564,9 +1582,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 0.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/seamount/layer/MOM_parameter_doc.all b/ocean_only/seamount/layer/MOM_parameter_doc.all index b6dcaafc2..1f219ae51 100644 --- a/ocean_only/seamount/layer/MOM_parameter_doc.all +++ b/ocean_only/seamount/layer/MOM_parameter_doc.all @@ -621,12 +621,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -643,6 +661,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -746,9 +767,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1483,9 +1501,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 0.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/seamount/rho/MOM_parameter_doc.all b/ocean_only/seamount/rho/MOM_parameter_doc.all index 554e04f2d..5f8ddf1c7 100644 --- a/ocean_only/seamount/rho/MOM_parameter_doc.all +++ b/ocean_only/seamount/rho/MOM_parameter_doc.all @@ -785,12 +785,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -807,6 +825,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -910,9 +931,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1643,9 +1661,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 0.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/seamount/sigma/MOM_parameter_doc.all b/ocean_only/seamount/sigma/MOM_parameter_doc.all index bd933bdcc..1d722f91f 100644 --- a/ocean_only/seamount/sigma/MOM_parameter_doc.all +++ b/ocean_only/seamount/sigma/MOM_parameter_doc.all @@ -734,12 +734,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -756,6 +774,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -859,9 +880,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1592,9 +1610,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 0.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/seamount/z/MOM_parameter_doc.all b/ocean_only/seamount/z/MOM_parameter_doc.all index 6a26cac6d..a890b2cf6 100644 --- a/ocean_only/seamount/z/MOM_parameter_doc.all +++ b/ocean_only/seamount/z/MOM_parameter_doc.all @@ -734,12 +734,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -756,6 +774,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -859,9 +880,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1592,9 +1610,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 0.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/single_column/BML/MOM_parameter_doc.all b/ocean_only/single_column/BML/MOM_parameter_doc.all index df42f679d..f70b46eb0 100644 --- a/ocean_only/single_column/BML/MOM_parameter_doc.all +++ b/ocean_only/single_column/BML/MOM_parameter_doc.all @@ -613,12 +613,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -635,6 +653,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -738,9 +759,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1466,9 +1484,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 600.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/single_column/EPBL/MOM_parameter_doc.all b/ocean_only/single_column/EPBL/MOM_parameter_doc.all index 42e100582..f33c69fc0 100644 --- a/ocean_only/single_column/EPBL/MOM_parameter_doc.all +++ b/ocean_only/single_column/EPBL/MOM_parameter_doc.all @@ -683,12 +683,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -705,6 +723,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -808,9 +829,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1618,9 +1636,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 600.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/single_column/KPP/MOM_parameter_doc.all b/ocean_only/single_column/KPP/MOM_parameter_doc.all index 3c9cbcdf8..511592c18 100644 --- a/ocean_only/single_column/KPP/MOM_parameter_doc.all +++ b/ocean_only/single_column/KPP/MOM_parameter_doc.all @@ -683,12 +683,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -705,6 +723,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -808,9 +829,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1540,9 +1558,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 600.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/sloshing/layer/MOM_parameter_doc.all b/ocean_only/sloshing/layer/MOM_parameter_doc.all index 77ea1b571..fae0fc513 100644 --- a/ocean_only/sloshing/layer/MOM_parameter_doc.all +++ b/ocean_only/sloshing/layer/MOM_parameter_doc.all @@ -602,12 +602,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -624,6 +642,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -727,9 +748,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1466,9 +1484,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 0.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/sloshing/rho/MOM_parameter_doc.all b/ocean_only/sloshing/rho/MOM_parameter_doc.all index e511fc0a3..8364608e9 100644 --- a/ocean_only/sloshing/rho/MOM_parameter_doc.all +++ b/ocean_only/sloshing/rho/MOM_parameter_doc.all @@ -768,12 +768,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -790,6 +808,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -893,9 +914,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1628,9 +1646,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 0.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/sloshing/z/MOM_parameter_doc.all b/ocean_only/sloshing/z/MOM_parameter_doc.all index 68e45f678..b25c89520 100644 --- a/ocean_only/sloshing/z/MOM_parameter_doc.all +++ b/ocean_only/sloshing/z/MOM_parameter_doc.all @@ -720,12 +720,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -742,6 +760,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -845,9 +866,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1580,9 +1598,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 0.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/torus_advection_test/MOM_parameter_doc.all b/ocean_only/torus_advection_test/MOM_parameter_doc.all index 99c86a74d..999deec8f 100644 --- a/ocean_only/torus_advection_test/MOM_parameter_doc.all +++ b/ocean_only/torus_advection_test/MOM_parameter_doc.all @@ -606,12 +606,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -628,6 +646,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -710,9 +731,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1431,9 +1449,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 0.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/tracer_mixing/rho/MOM_parameter_doc.all b/ocean_only/tracer_mixing/rho/MOM_parameter_doc.all index 02937e2ad..e9118ce6e 100644 --- a/ocean_only/tracer_mixing/rho/MOM_parameter_doc.all +++ b/ocean_only/tracer_mixing/rho/MOM_parameter_doc.all @@ -769,12 +769,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -791,6 +809,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -894,9 +915,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1629,9 +1647,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 1.0E+04 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/tracer_mixing/z/MOM_parameter_doc.all b/ocean_only/tracer_mixing/z/MOM_parameter_doc.all index e806a1285..531e463f4 100644 --- a/ocean_only/tracer_mixing/z/MOM_parameter_doc.all +++ b/ocean_only/tracer_mixing/z/MOM_parameter_doc.all @@ -721,12 +721,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -743,6 +761,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -846,9 +867,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -1581,9 +1599,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 1.0E+04 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/ocean_only/unit_tests/MOM_parameter_doc.all b/ocean_only/unit_tests/MOM_parameter_doc.all index f33230a12..6f662b130 100644 --- a/ocean_only/unit_tests/MOM_parameter_doc.all +++ b/ocean_only/unit_tests/MOM_parameter_doc.all @@ -485,12 +485,30 @@ RESOLN_USE_EBT = False ! [Boolean] default = False BACKSCAT_EBT_POWER = 0.0 ! [nondim] default = 0.0 ! Power to raise EBT vertical structure to when backscatter has vertical ! structure. +BS_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, the SQG vertical structure is used for backscatter on the condition + ! that BS_EBT_power=0 +SQG_EXPO = 1.0 ! [nondim] default = 1.0 + ! Nondimensional exponent coeffecient of the SQG mode that is used for the + ! vertical struture of diffusivities. KHTH_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! thickness diffusivity. +KHTH_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of thickness diffusivity. +KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! tracer diffusivity. +KHTR_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the surface quasigeostrophic structure as the vertical structure + ! of tracer diffusivity. KD_GL90_USE_EBT_STRUCT = False ! [Boolean] default = False ! If true, uses the equivalent barotropic structure as the vertical structure of ! diffusivity in the GL90 scheme. +KD_GL90_USE_SQG_STRUCT = False ! [Boolean] default = False + ! If true, uses the equivalent barotropic structure as the vertical structure of + ! diffusivity in the GL90 scheme. KHTH_SLOPE_CFF = 0.0 ! [nondim] default = 0.0 ! The nondimensional coefficient in the Visbeck formula for the interface depth ! diffusivity @@ -507,6 +525,9 @@ VERY_SMALL_FREQUENCY = 1.0E-17 ! [s-1] default = 1.0E-17 USE_STANLEY_ISO = False ! [Boolean] default = False ! If true, turn on Stanley SGS T variance parameterization in isopycnal slope ! code. +KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 + ! A diapycnal diffusivity that is used to interpolate more sensible values of T + ! & S into thin layers. USE_QG_LEITH_GM = False ! [Boolean] default = False ! If true, use the QG Leith viscosity as the GM coefficient. @@ -587,9 +608,6 @@ DETANGLE_INTERFACES = False ! [Boolean] default = False KHTH_SLOPE_MAX = 0.01 ! [nondim] default = 0.01 ! A slope beyond which the calculated isopycnal slope is not reliable and is ! scaled away. -KD_SMOOTH = 1.0E-06 ! [m2 s-1] default = 1.0E-06 - ! A diapycnal diffusivity that is used to interpolate more sensible values of T - ! & S into thin layers. KHTH_USE_FGNV_STREAMFUNCTION = False ! [Boolean] default = False ! If true, use the streamfunction formulation of Ferrari et al., 2010, which ! effectively emphasizes graver vertical modes by smoothing in the vertical. @@ -902,9 +920,6 @@ TRACER_ADVECTION_SCHEME = "PLM" ! default = "PLM" ! === module MOM_tracer_hor_diff === KHTR = 0.0 ! [m2 s-1] default = 0.0 ! The background along-isopycnal tracer diffusivity. -KHTR_USE_EBT_STRUCT = False ! [Boolean] default = False - ! If true, uses the equivalent barotropic structure as the vertical structure of - ! the tracer diffusivity. KHTR_MIN = 0.0 ! [m2 s-1] default = 0.0 ! The minimum along-isopycnal tracer diffusivity. KHTR_MAX = 0.0 ! [m2 s-1] default = 0.0 diff --git a/src/MOM6 b/src/MOM6 index dbb360197..7a9adbcac 160000 --- a/src/MOM6 +++ b/src/MOM6 @@ -1 +1 @@ -Subproject commit dbb360197fd6c0a3f5ab2d51c10873f0c352d59c +Subproject commit 7a9adbcac5259be8fde7b22dcc2cc06b8d3e8283