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 45af20aa5..bb79e486d 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 @@ -866,6 +866,13 @@ DRAG_AS_BODY_FORCE = False ! [Boolean] default = False CHANNEL_DRAG = True ! [Boolean] default = False ! If true, the bottom drag is exerted directly on each layer proportional to the ! fraction of the bottom it overlies. +CHANNEL_DRAG_SHELFBREAK_DEPTH = 0.0 ! [m] default = 0.0 + ! When CHANNEL_DRAG is true, the bathymetric depth interpolated to the vorticity + ! point is a combination of the harmonic mean of the adjacent velocity point + ! depths below this depth and the arithmetic mean of the depths above it, to + ! roughly mimic a continental shelf break profile. Setting this to exceed + ! MAXIMUM_DEPTH leads to linear interpolation of the topography between velocity + ! points. LINEAR_DRAG = False ! [Boolean] default = False ! If LINEAR_DRAG and BOTTOMDRAGLAW are defined the drag law is ! cdrag*DRAG_BG_VEL*u. 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 749b29a2b..dc1b8c490 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 @@ -866,6 +866,13 @@ DRAG_AS_BODY_FORCE = False ! [Boolean] default = False CHANNEL_DRAG = True ! [Boolean] default = False ! If true, the bottom drag is exerted directly on each layer proportional to the ! fraction of the bottom it overlies. +CHANNEL_DRAG_SHELFBREAK_DEPTH = 0.0 ! [m] default = 0.0 + ! When CHANNEL_DRAG is true, the bathymetric depth interpolated to the vorticity + ! point is a combination of the harmonic mean of the adjacent velocity point + ! depths below this depth and the arithmetic mean of the depths above it, to + ! roughly mimic a continental shelf break profile. Setting this to exceed + ! MAXIMUM_DEPTH leads to linear interpolation of the topography between velocity + ! points. LINEAR_DRAG = False ! [Boolean] default = False ! If LINEAR_DRAG and BOTTOMDRAGLAW are defined the drag law is ! cdrag*DRAG_BG_VEL*u. 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 9bf533fe1..451affb36 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 @@ -866,6 +866,13 @@ DRAG_AS_BODY_FORCE = False ! [Boolean] default = False CHANNEL_DRAG = True ! [Boolean] default = False ! If true, the bottom drag is exerted directly on each layer proportional to the ! fraction of the bottom it overlies. +CHANNEL_DRAG_SHELFBREAK_DEPTH = 0.0 ! [m] default = 0.0 + ! When CHANNEL_DRAG is true, the bathymetric depth interpolated to the vorticity + ! point is a combination of the harmonic mean of the adjacent velocity point + ! depths below this depth and the arithmetic mean of the depths above it, to + ! roughly mimic a continental shelf break profile. Setting this to exceed + ! MAXIMUM_DEPTH leads to linear interpolation of the topography between velocity + ! points. LINEAR_DRAG = False ! [Boolean] default = False ! If LINEAR_DRAG and BOTTOMDRAGLAW are defined the drag law is ! cdrag*DRAG_BG_VEL*u. diff --git a/ice_ocean_SIS2/Baltic/MOM_parameter_doc.all b/ice_ocean_SIS2/Baltic/MOM_parameter_doc.all index f725db658..7b18072d9 100644 --- a/ice_ocean_SIS2/Baltic/MOM_parameter_doc.all +++ b/ice_ocean_SIS2/Baltic/MOM_parameter_doc.all @@ -866,6 +866,13 @@ DRAG_AS_BODY_FORCE = False ! [Boolean] default = False CHANNEL_DRAG = True ! [Boolean] default = False ! If true, the bottom drag is exerted directly on each layer proportional to the ! fraction of the bottom it overlies. +CHANNEL_DRAG_SHELFBREAK_DEPTH = 0.0 ! [m] default = 0.0 + ! When CHANNEL_DRAG is true, the bathymetric depth interpolated to the vorticity + ! point is a combination of the harmonic mean of the adjacent velocity point + ! depths below this depth and the arithmetic mean of the depths above it, to + ! roughly mimic a continental shelf break profile. Setting this to exceed + ! MAXIMUM_DEPTH leads to linear interpolation of the topography between velocity + ! points. LINEAR_DRAG = False ! [Boolean] default = False ! If LINEAR_DRAG and BOTTOMDRAGLAW are defined the drag law is ! cdrag*DRAG_BG_VEL*u. 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 1e9b816e0..dd076701d 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 @@ -1067,6 +1067,13 @@ DRAG_AS_BODY_FORCE = False ! [Boolean] default = False CHANNEL_DRAG = True ! [Boolean] default = False ! If true, the bottom drag is exerted directly on each layer proportional to the ! fraction of the bottom it overlies. +CHANNEL_DRAG_SHELFBREAK_DEPTH = 0.0 ! [m] default = 0.0 + ! When CHANNEL_DRAG is true, the bathymetric depth interpolated to the vorticity + ! point is a combination of the harmonic mean of the adjacent velocity point + ! depths below this depth and the arithmetic mean of the depths above it, to + ! roughly mimic a continental shelf break profile. Setting this to exceed + ! MAXIMUM_DEPTH leads to linear interpolation of the topography between velocity + ! points. LINEAR_DRAG = False ! [Boolean] default = False ! If LINEAR_DRAG and BOTTOMDRAGLAW are defined the drag law is ! cdrag*DRAG_BG_VEL*u. 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 decceb57e..6bd0eca27 100644 --- a/ice_ocean_SIS2/Baltic_OM4_025/MOM_parameter_doc.all +++ b/ice_ocean_SIS2/Baltic_OM4_025/MOM_parameter_doc.all @@ -1185,6 +1185,13 @@ DRAG_AS_BODY_FORCE = False ! [Boolean] default = False CHANNEL_DRAG = True ! [Boolean] default = False ! If true, the bottom drag is exerted directly on each layer proportional to the ! fraction of the bottom it overlies. +CHANNEL_DRAG_SHELFBREAK_DEPTH = 0.0 ! [m] default = 0.0 + ! When CHANNEL_DRAG is true, the bathymetric depth interpolated to the vorticity + ! point is a combination of the harmonic mean of the adjacent velocity point + ! depths below this depth and the arithmetic mean of the depths above it, to + ! roughly mimic a continental shelf break profile. Setting this to exceed + ! MAXIMUM_DEPTH leads to linear interpolation of the topography between velocity + ! points. LINEAR_DRAG = False ! [Boolean] default = False ! If LINEAR_DRAG and BOTTOMDRAGLAW are defined the drag law is ! cdrag*DRAG_BG_VEL*u. 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 4494029c6..d0b00fb0e 100644 --- a/ice_ocean_SIS2/Baltic_OM4_05/MOM_parameter_doc.all +++ b/ice_ocean_SIS2/Baltic_OM4_05/MOM_parameter_doc.all @@ -1189,6 +1189,13 @@ DRAG_AS_BODY_FORCE = False ! [Boolean] default = False CHANNEL_DRAG = True ! [Boolean] default = False ! If true, the bottom drag is exerted directly on each layer proportional to the ! fraction of the bottom it overlies. +CHANNEL_DRAG_SHELFBREAK_DEPTH = 0.0 ! [m] default = 0.0 + ! When CHANNEL_DRAG is true, the bathymetric depth interpolated to the vorticity + ! point is a combination of the harmonic mean of the adjacent velocity point + ! depths below this depth and the arithmetic mean of the depths above it, to + ! roughly mimic a continental shelf break profile. Setting this to exceed + ! MAXIMUM_DEPTH leads to linear interpolation of the topography between velocity + ! points. LINEAR_DRAG = False ! [Boolean] default = False ! If LINEAR_DRAG and BOTTOMDRAGLAW are defined the drag law is ! cdrag*DRAG_BG_VEL*u. diff --git a/ice_ocean_SIS2/Baltic_OM5_025/MOM_parameter_doc.all b/ice_ocean_SIS2/Baltic_OM5_025/MOM_parameter_doc.all index 8b643941b..8bd2fd5d2 100644 --- a/ice_ocean_SIS2/Baltic_OM5_025/MOM_parameter_doc.all +++ b/ice_ocean_SIS2/Baltic_OM5_025/MOM_parameter_doc.all @@ -1172,6 +1172,13 @@ DRAG_AS_BODY_FORCE = False ! [Boolean] default = False CHANNEL_DRAG = True ! [Boolean] default = False ! If true, the bottom drag is exerted directly on each layer proportional to the ! fraction of the bottom it overlies. +CHANNEL_DRAG_SHELFBREAK_DEPTH = 0.0 ! [m] default = 0.0 + ! When CHANNEL_DRAG is true, the bathymetric depth interpolated to the vorticity + ! point is a combination of the harmonic mean of the adjacent velocity point + ! depths below this depth and the arithmetic mean of the depths above it, to + ! roughly mimic a continental shelf break profile. Setting this to exceed + ! MAXIMUM_DEPTH leads to linear interpolation of the topography between velocity + ! points. LINEAR_DRAG = False ! [Boolean] default = False ! If LINEAR_DRAG and BOTTOMDRAGLAW are defined the drag law is ! cdrag*DRAG_BG_VEL*u. diff --git a/ice_ocean_SIS2/Baltic_OM5nb_025/MOM_parameter_doc.all b/ice_ocean_SIS2/Baltic_OM5nb_025/MOM_parameter_doc.all index f589585dc..0fe07dc2b 100644 --- a/ice_ocean_SIS2/Baltic_OM5nb_025/MOM_parameter_doc.all +++ b/ice_ocean_SIS2/Baltic_OM5nb_025/MOM_parameter_doc.all @@ -1164,6 +1164,13 @@ DRAG_AS_BODY_FORCE = False ! [Boolean] default = False CHANNEL_DRAG = True ! [Boolean] default = False ! If true, the bottom drag is exerted directly on each layer proportional to the ! fraction of the bottom it overlies. +CHANNEL_DRAG_SHELFBREAK_DEPTH = 0.0 ! [m] default = 0.0 + ! When CHANNEL_DRAG is true, the bathymetric depth interpolated to the vorticity + ! point is a combination of the harmonic mean of the adjacent velocity point + ! depths below this depth and the arithmetic mean of the depths above it, to + ! roughly mimic a continental shelf break profile. Setting this to exceed + ! MAXIMUM_DEPTH leads to linear interpolation of the topography between velocity + ! points. LINEAR_DRAG = False ! [Boolean] default = False ! If LINEAR_DRAG and BOTTOMDRAGLAW are defined the drag law is ! cdrag*DRAG_BG_VEL*u. diff --git a/ice_ocean_SIS2/OM4_025/MOM_parameter_doc.all b/ice_ocean_SIS2/OM4_025/MOM_parameter_doc.all index 26bb88707..e60dac4bb 100644 --- a/ice_ocean_SIS2/OM4_025/MOM_parameter_doc.all +++ b/ice_ocean_SIS2/OM4_025/MOM_parameter_doc.all @@ -1185,6 +1185,13 @@ DRAG_AS_BODY_FORCE = False ! [Boolean] default = False CHANNEL_DRAG = True ! [Boolean] default = False ! If true, the bottom drag is exerted directly on each layer proportional to the ! fraction of the bottom it overlies. +CHANNEL_DRAG_SHELFBREAK_DEPTH = 0.0 ! [m] default = 0.0 + ! When CHANNEL_DRAG is true, the bathymetric depth interpolated to the vorticity + ! point is a combination of the harmonic mean of the adjacent velocity point + ! depths below this depth and the arithmetic mean of the depths above it, to + ! roughly mimic a continental shelf break profile. Setting this to exceed + ! MAXIMUM_DEPTH leads to linear interpolation of the topography between velocity + ! points. LINEAR_DRAG = False ! [Boolean] default = False ! If LINEAR_DRAG and BOTTOMDRAGLAW are defined the drag law is ! cdrag*DRAG_BG_VEL*u. diff --git a/ice_ocean_SIS2/OM4_05/MOM_parameter_doc.all b/ice_ocean_SIS2/OM4_05/MOM_parameter_doc.all index 22f2ff312..6254c696b 100644 --- a/ice_ocean_SIS2/OM4_05/MOM_parameter_doc.all +++ b/ice_ocean_SIS2/OM4_05/MOM_parameter_doc.all @@ -1189,6 +1189,13 @@ DRAG_AS_BODY_FORCE = False ! [Boolean] default = False CHANNEL_DRAG = True ! [Boolean] default = False ! If true, the bottom drag is exerted directly on each layer proportional to the ! fraction of the bottom it overlies. +CHANNEL_DRAG_SHELFBREAK_DEPTH = 0.0 ! [m] default = 0.0 + ! When CHANNEL_DRAG is true, the bathymetric depth interpolated to the vorticity + ! point is a combination of the harmonic mean of the adjacent velocity point + ! depths below this depth and the arithmetic mean of the depths above it, to + ! roughly mimic a continental shelf break profile. Setting this to exceed + ! MAXIMUM_DEPTH leads to linear interpolation of the topography between velocity + ! points. LINEAR_DRAG = False ! [Boolean] default = False ! If LINEAR_DRAG and BOTTOMDRAGLAW are defined the drag law is ! cdrag*DRAG_BG_VEL*u. diff --git a/ice_ocean_SIS2/OM_1deg/MOM_parameter_doc.all b/ice_ocean_SIS2/OM_1deg/MOM_parameter_doc.all index d22d6d0c6..2ae43c537 100644 --- a/ice_ocean_SIS2/OM_1deg/MOM_parameter_doc.all +++ b/ice_ocean_SIS2/OM_1deg/MOM_parameter_doc.all @@ -1176,6 +1176,13 @@ DRAG_AS_BODY_FORCE = False ! [Boolean] default = False CHANNEL_DRAG = True ! [Boolean] default = False ! If true, the bottom drag is exerted directly on each layer proportional to the ! fraction of the bottom it overlies. +CHANNEL_DRAG_SHELFBREAK_DEPTH = 0.0 ! [m] default = 0.0 + ! When CHANNEL_DRAG is true, the bathymetric depth interpolated to the vorticity + ! point is a combination of the harmonic mean of the adjacent velocity point + ! depths below this depth and the arithmetic mean of the depths above it, to + ! roughly mimic a continental shelf break profile. Setting this to exceed + ! MAXIMUM_DEPTH leads to linear interpolation of the topography between velocity + ! points. LINEAR_DRAG = False ! [Boolean] default = False ! If LINEAR_DRAG and BOTTOMDRAGLAW are defined the drag law is ! cdrag*DRAG_BG_VEL*u. diff --git a/ice_ocean_SIS2/SIS2/MOM_parameter_doc.all b/ice_ocean_SIS2/SIS2/MOM_parameter_doc.all index 3d6230fd8..8d632aaee 100644 --- a/ice_ocean_SIS2/SIS2/MOM_parameter_doc.all +++ b/ice_ocean_SIS2/SIS2/MOM_parameter_doc.all @@ -837,6 +837,13 @@ DRAG_AS_BODY_FORCE = False ! [Boolean] default = False CHANNEL_DRAG = True ! [Boolean] default = False ! If true, the bottom drag is exerted directly on each layer proportional to the ! fraction of the bottom it overlies. +CHANNEL_DRAG_SHELFBREAK_DEPTH = 0.0 ! [m] default = 0.0 + ! When CHANNEL_DRAG is true, the bathymetric depth interpolated to the vorticity + ! point is a combination of the harmonic mean of the adjacent velocity point + ! depths below this depth and the arithmetic mean of the depths above it, to + ! roughly mimic a continental shelf break profile. Setting this to exceed + ! MAXIMUM_DEPTH leads to linear interpolation of the topography between velocity + ! points. LINEAR_DRAG = False ! [Boolean] default = False ! If LINEAR_DRAG and BOTTOMDRAGLAW are defined the drag law is ! cdrag*DRAG_BG_VEL*u. 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 65384a669..4aa0f01eb 100644 --- a/ice_ocean_SIS2/SIS2_bergs_cgrid/MOM_parameter_doc.all +++ b/ice_ocean_SIS2/SIS2_bergs_cgrid/MOM_parameter_doc.all @@ -837,6 +837,13 @@ DRAG_AS_BODY_FORCE = False ! [Boolean] default = False CHANNEL_DRAG = True ! [Boolean] default = False ! If true, the bottom drag is exerted directly on each layer proportional to the ! fraction of the bottom it overlies. +CHANNEL_DRAG_SHELFBREAK_DEPTH = 0.0 ! [m] default = 0.0 + ! When CHANNEL_DRAG is true, the bathymetric depth interpolated to the vorticity + ! point is a combination of the harmonic mean of the adjacent velocity point + ! depths below this depth and the arithmetic mean of the depths above it, to + ! roughly mimic a continental shelf break profile. Setting this to exceed + ! MAXIMUM_DEPTH leads to linear interpolation of the topography between velocity + ! points. LINEAR_DRAG = False ! [Boolean] default = False ! If LINEAR_DRAG and BOTTOMDRAGLAW are defined the drag law is ! cdrag*DRAG_BG_VEL*u. diff --git a/ice_ocean_SIS2/SIS2_cgrid/MOM_parameter_doc.all b/ice_ocean_SIS2/SIS2_cgrid/MOM_parameter_doc.all index a892850a3..e58588e43 100644 --- a/ice_ocean_SIS2/SIS2_cgrid/MOM_parameter_doc.all +++ b/ice_ocean_SIS2/SIS2_cgrid/MOM_parameter_doc.all @@ -837,6 +837,13 @@ DRAG_AS_BODY_FORCE = False ! [Boolean] default = False CHANNEL_DRAG = True ! [Boolean] default = False ! If true, the bottom drag is exerted directly on each layer proportional to the ! fraction of the bottom it overlies. +CHANNEL_DRAG_SHELFBREAK_DEPTH = 0.0 ! [m] default = 0.0 + ! When CHANNEL_DRAG is true, the bathymetric depth interpolated to the vorticity + ! point is a combination of the harmonic mean of the adjacent velocity point + ! depths below this depth and the arithmetic mean of the depths above it, to + ! roughly mimic a continental shelf break profile. Setting this to exceed + ! MAXIMUM_DEPTH leads to linear interpolation of the topography between velocity + ! points. LINEAR_DRAG = False ! [Boolean] default = False ! If LINEAR_DRAG and BOTTOMDRAGLAW are defined the drag law is ! cdrag*DRAG_BG_VEL*u. diff --git a/ocean_only/global_ALE/hycom/MOM_parameter_doc.all b/ocean_only/global_ALE/hycom/MOM_parameter_doc.all index b4e6c05b9..4b4071674 100644 --- a/ocean_only/global_ALE/hycom/MOM_parameter_doc.all +++ b/ocean_only/global_ALE/hycom/MOM_parameter_doc.all @@ -1114,6 +1114,13 @@ DRAG_AS_BODY_FORCE = False ! [Boolean] default = False CHANNEL_DRAG = True ! [Boolean] default = False ! If true, the bottom drag is exerted directly on each layer proportional to the ! fraction of the bottom it overlies. +CHANNEL_DRAG_SHELFBREAK_DEPTH = 0.0 ! [m] default = 0.0 + ! When CHANNEL_DRAG is true, the bathymetric depth interpolated to the vorticity + ! point is a combination of the harmonic mean of the adjacent velocity point + ! depths below this depth and the arithmetic mean of the depths above it, to + ! roughly mimic a continental shelf break profile. Setting this to exceed + ! MAXIMUM_DEPTH leads to linear interpolation of the topography between velocity + ! points. LINEAR_DRAG = False ! [Boolean] default = False ! If LINEAR_DRAG and BOTTOMDRAGLAW are defined the drag law is ! cdrag*DRAG_BG_VEL*u. diff --git a/ocean_only/global_ALE/layer/MOM_parameter_doc.all b/ocean_only/global_ALE/layer/MOM_parameter_doc.all index 8137c6f06..01579c10c 100644 --- a/ocean_only/global_ALE/layer/MOM_parameter_doc.all +++ b/ocean_only/global_ALE/layer/MOM_parameter_doc.all @@ -968,6 +968,13 @@ DRAG_AS_BODY_FORCE = False ! [Boolean] default = False CHANNEL_DRAG = True ! [Boolean] default = False ! If true, the bottom drag is exerted directly on each layer proportional to the ! fraction of the bottom it overlies. +CHANNEL_DRAG_SHELFBREAK_DEPTH = 0.0 ! [m] default = 0.0 + ! When CHANNEL_DRAG is true, the bathymetric depth interpolated to the vorticity + ! point is a combination of the harmonic mean of the adjacent velocity point + ! depths below this depth and the arithmetic mean of the depths above it, to + ! roughly mimic a continental shelf break profile. Setting this to exceed + ! MAXIMUM_DEPTH leads to linear interpolation of the topography between velocity + ! points. LINEAR_DRAG = False ! [Boolean] default = False ! If LINEAR_DRAG and BOTTOMDRAGLAW are defined the drag law is ! cdrag*DRAG_BG_VEL*u. diff --git a/ocean_only/global_ALE/z/MOM_parameter_doc.all b/ocean_only/global_ALE/z/MOM_parameter_doc.all index caf8463f3..5bf7fea7f 100644 --- a/ocean_only/global_ALE/z/MOM_parameter_doc.all +++ b/ocean_only/global_ALE/z/MOM_parameter_doc.all @@ -1054,6 +1054,13 @@ DRAG_AS_BODY_FORCE = False ! [Boolean] default = False CHANNEL_DRAG = True ! [Boolean] default = False ! If true, the bottom drag is exerted directly on each layer proportional to the ! fraction of the bottom it overlies. +CHANNEL_DRAG_SHELFBREAK_DEPTH = 0.0 ! [m] default = 0.0 + ! When CHANNEL_DRAG is true, the bathymetric depth interpolated to the vorticity + ! point is a combination of the harmonic mean of the adjacent velocity point + ! depths below this depth and the arithmetic mean of the depths above it, to + ! roughly mimic a continental shelf break profile. Setting this to exceed + ! MAXIMUM_DEPTH leads to linear interpolation of the topography between velocity + ! points. LINEAR_DRAG = False ! [Boolean] default = False ! If LINEAR_DRAG and BOTTOMDRAGLAW are defined the drag law is ! cdrag*DRAG_BG_VEL*u. diff --git a/ocean_only/nonBous_global/MOM_parameter_doc.all b/ocean_only/nonBous_global/MOM_parameter_doc.all index 74574ba2d..188666bb2 100644 --- a/ocean_only/nonBous_global/MOM_parameter_doc.all +++ b/ocean_only/nonBous_global/MOM_parameter_doc.all @@ -789,6 +789,13 @@ DRAG_AS_BODY_FORCE = False ! [Boolean] default = False CHANNEL_DRAG = True ! [Boolean] default = False ! If true, the bottom drag is exerted directly on each layer proportional to the ! fraction of the bottom it overlies. +CHANNEL_DRAG_SHELFBREAK_DEPTH = 0.0 ! [m] default = 0.0 + ! When CHANNEL_DRAG is true, the bathymetric depth interpolated to the vorticity + ! point is a combination of the harmonic mean of the adjacent velocity point + ! depths below this depth and the arithmetic mean of the depths above it, to + ! roughly mimic a continental shelf break profile. Setting this to exceed + ! MAXIMUM_DEPTH leads to linear interpolation of the topography between velocity + ! points. LINEAR_DRAG = False ! [Boolean] default = False ! If LINEAR_DRAG and BOTTOMDRAGLAW are defined the drag law is ! cdrag*DRAG_BG_VEL*u. diff --git a/src/MOM6 b/src/MOM6 index 0f26d6958..67f7637d9 160000 --- a/src/MOM6 +++ b/src/MOM6 @@ -1 +1 @@ -Subproject commit 0f26d6958423d894823e0db79c6f9bfee64b0bfa +Subproject commit 67f7637d9b98effe0189a46412f4a0b4c0113de5