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MOM6: Merge branch 'gustavo-marques-dev-ncar-candidate-2018-09-26' in…
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…to dev/master

PR from NCAR:
- NOAA-GFDL/MOM6@c77ad425c Merge branch 'gustavo-marques-dev-ncar-candidate-2018-09-26' into dev/master
- NOAA-GFDL/MOM6@c09a6611a Merge pull request #4 from alperaltuntas/bkgnd_mixing_fix
- NOAA-GFDL/MOM6@3666d609d read prandtl_bknd for all cases
- NOAA-GFDL/MOM6@4306feb4b  end if to endif and end do to enddo
- NOAA-GFDL/MOM6@3714a3955 un-indent subroutines
- NOAA-GFDL/MOM6@caec6dd27 read prandtl_bkgnd only for cvmix or horiz_varying_background
- NOAA-GFDL/MOM6@f91944488 fix divide by error if Kd=0.0
- NOAA-GFDL/MOM6@67b041352 Merge pull request #4 from NCAR/dev/ncar
- NOAA-GFDL/MOM6@bf44b18b5 Merge branch 'dev/master' into dev-ncar-candidate-2018-09-26
- NOAA-GFDL/MOM6@bcb195a83 Merge pull request #80 from gustavo-marques/pass_OBLD_caps
- NOAA-GFDL/MOM6@6f6f92a51 Change melt potential from time accumulated to instantaneous
- NOAA-GFDL/MOM6@9f0676e83 Copy Hml into sfc_state, so that caps can access it
- NOAA-GFDL/MOM6@6ccd94c73 Pass Hml, from ePBL or KPP, via a call to diabatic
- NOAA-GFDL/MOM6@405061779 Add OBLD into MCT cap
- NOAA-GFDL/MOM6@1ced255e0 Merge pull request #78 from gustavo-marques/update_melt_potential
- NOAA-GFDL/MOM6@d32386dc5 Allocates visc%MLD when hfreeze >= 0.0
- NOAA-GFDL/MOM6@ddccc44c9 Copy OBLD to visc%MLD when using KPP
- NOAA-GFDL/MOM6@d3d8215bd Add a new implementation for the melt potential calculation
- NOAA-GFDL/MOM6@f1445de5f Add option to use melt potential in mct and couple_driver
- NOAA-GFDL/MOM6@9c8b3c5da Comment DEBUG message
- NOAA-GFDL/MOM6@b7d83affc Merge pull request #73 from alperaltuntas/horiz_varying_background
- NOAA-GFDL/MOM6@4a7de48ad Merge pull request #77 from gustavo-marques/add_melt_potential_mct
- NOAA-GFDL/MOM6@5d6ff165f Merge branch 'dev/ncar' into add_melt_potential_mct
- NOAA-GFDL/MOM6@d0bc3bc2f Fix bug and make sure melt potential is always <= 0
- NOAA-GFDL/MOM6@c6b253400 Pass melt/freeze potential to coupler; reset melt_potential
- NOAA-GFDL/MOM6@eb2c69f1d Replace units (W/m^2 to J/m^2) in the comments
- NOAA-GFDL/MOM6@be0e7a844 Remove dt from extract_surface_state
- NOAA-GFDL/MOM6@12011dec9 Merge pull request #76 from gustavo-marques/merge-candidate-2018-07-16
- NOAA-GFDL/MOM6@05d6c805a Update melt_potential again, but values are still ~ 3 x smaller
- NOAA-GFDL/MOM6@0a55527b0 Merge branch 'dev/ncar' into merge-candidate-2018-07-16
- NOAA-GFDL/MOM6@7347ad973 Update calculation of melt_potential
- NOAA-GFDL/MOM6@4e5bf7494 Change calculation of melt_potential
- NOAA-GFDL/MOM6@60eb7ec30 Add comment about icefrq used in Hycom
- NOAA-GFDL/MOM6@d981745f8 Fix a call to ocn_export
- NOAA-GFDL/MOM6@b52db1ff5 Allocate/deallocate melt_potential
- NOAA-GFDL/MOM6@3cdd97bfa Add option to calculate melt potential
- NOAA-GFDL/MOM6@a840dc0f4 Pass melt potential (o2x_Fioo_q) via mct driver
- NOAA-GFDL/MOM6@4e41df988 Merge pull request #3 from NCAR/dev/ncar
- NOAA-GFDL/MOM6@02d9be2f9 rm temporarily the noupc cap
- NOAA-GFDL/MOM6@04845d4e8 Merge pull request #74 from NCAR/dev/nuopc
- NOAA-GFDL/MOM6@25873994d rename mom_cap
- NOAA-GFDL/MOM6@353f60f07 Merge pull request #75 from NCAR/dev/nuopc_alper
- NOAA-GFDL/MOM6@0cdce0817 Merge branch 'dev-master-candidate-2018-07-16' into merge-candidate-2018-07-16
- NOAA-GFDL/MOM6@116fdfba4 rm trailing spaces
- NOAA-GFDL/MOM6@838de5293 improve mct cap doxumentation
- NOAA-GFDL/MOM6@290d4f5e4 add only keywords
- NOAA-GFDL/MOM6@ad1a2957d limit line widths to 120 chars
- NOAA-GFDL/MOM6@a2c6a7a2f improve tab width consistency
- NOAA-GFDL/MOM6@c2655b3ab fix call to shelf_calc_flux
- NOAA-GFDL/MOM6@8606be9df removed more trailing white space
- NOAA-GFDL/MOM6@d32333e07 fixed trailing white space
- NOAA-GFDL/MOM6@7fb01ffe9 removed trailing whitespace
- NOAA-GFDL/MOM6@f49c205eb more cleanup of cesm cap
- NOAA-GFDL/MOM6@450f87cbc more changes to get the nuopc cap working
- NOAA-GFDL/MOM6@403f59a8c changes needed to get nuopc cap restarting correctly
- NOAA-GFDL/MOM6@6f43605f9 removed use for shr_flds_dom_coord and shr_flds_dom_other by hardwiring names
- NOAA-GFDL/MOM6@2d89fa416 merged to head of dev/ncar
- NOAA-GFDL/MOM6@62dea759f updates for get nuopc working
- NOAA-GFDL/MOM6@bd90705ea Merge pull request #72 from gustavo-marques/update_KPP
- NOAA-GFDL/MOM6@ebceaece5 add horiz_varying_background scheme
- NOAA-GFDL/MOM6@48845179f check whether KD, KV and PRANDTL_BKGND are compatible
- NOAA-GFDL/MOM6@4b2bd2f13 Merge branch 'kpp_changes' into horiz_varying_background
- NOAA-GFDL/MOM6@1516d6a40 add safety checks for MOM_bkgnd_mixing schemes
- NOAA-GFDL/MOM6@7f67a4596 changes to get mom6 working correctly in nuopc mode and addition of debug output
- NOAA-GFDL/MOM6@c4f2a5e7f more updates
- NOAA-GFDL/MOM6@9e2578044 Merge branch 'dev/nuopc' of https://github.com/NCAR/MOM6 into dev/nuopc
- NOAA-GFDL/MOM6@50e4a654a additional changes to have mom cap nuopc working without a lot of diagnostic output
- NOAA-GFDL/MOM6@f3ca0c8df fixes to get mom cap working with cice
- NOAA-GFDL/MOM6@eef4bf2d4 Added global grid nx and ny scalars to MOM6 cap for writing history files
- NOAA-GFDL/MOM6@b7a88a6cc Merge branch 'mvertens/dev_nuopc' into dev/nuopc
- NOAA-GFDL/MOM6@4c1a97fc7 no longer need to scale by mask - since its done in MOM_surface_forcing
- NOAA-GFDL/MOM6@5f1b51c72 more cleanup of ocn_comp_mct
- NOAA-GFDL/MOM6@3d1962c01 changes to MOM6 to get nuopc and mct caps similar
- NOAA-GFDL/MOM6@b10f3434a last set of changes on the mct side to get mct and nuopc caps compatible
- NOAA-GFDL/MOM6@972293480 more updates to get nuopc and mct closer
- NOAA-GFDL/MOM6@f482863b3 more changes to bring in nuopc and mct caps closer together
- NOAA-GFDL/MOM6@8a230737d more udpates to make mct and mom caps similar
- NOAA-GFDL/MOM6@06565ec01 major refactor of mct interface - and addition -f MOM_ocean_model.F90 and MOM_surface_forcing.F90 to mct and nuopc cap codes
- NOAA-GFDL/MOM6@9fae628cd fixes for having mom6 work with nuopc-cmeps-v0.4
- NOAA-GFDL/MOM6@0a494857f Merge branch 'dev/ncar_nuopc' of https://github.com/mvertens/MOM6 into dev/nuopc
- NOAA-GFDL/MOM6@93d7a07bc changes to mom cap to be compatible with nuopcB_180413
- NOAA-GFDL/MOM6@fdc7962b5 updates for cesm-nuopc-cmeps-mom6-nems_cap configuration
- NOAA-GFDL/MOM6@d30900b26 update mom6 nuopc cap
- NOAA-GFDL/MOM6@2cfa6314a update mom_cap for cesm
- NOAA-GFDL/MOM6@5374582b3 update mom cap from NEMS
- NOAA-GFDL/MOM6@7bf531bf3 placed the GFDL MOM6 cap as a starting point in the new nuopc_driver/ directory
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adcroft committed Oct 5, 2018
1 parent 78cfb2d commit 585b9ce
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Showing 62 changed files with 660 additions and 178 deletions.
14 changes: 11 additions & 3 deletions coupled_AM2_LM3_SIS/CM2G63L/MOM_parameter_doc.all
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Original file line number Diff line number Diff line change
Expand Up @@ -75,6 +75,11 @@ THERMO_SPANS_COUPLING = False ! [Boolean] default = False
! The actual thermodynamic timestep that is used in this
! case is the largest integer multiple of the coupling
! timestep that is less than or equal to DT_THERM.
HFREEZE = -1.0 ! [m] default = -1.0
! If HFREEZE > 0, melt potential will be computed. The actual depth
! over which melt potential is computed will be min(HFREEZE, OBLD),
! where OBLD is the boundary layer depth. If HFREEZE <= 0 (default),
! melt potential will not be computed.
MIN_Z_DIAG_INTERVAL = 2.16E+04 ! [s] default = 0.0
! The minimum amount of time in seconds between
! calculations of depth-space diagnostics. Making this
Expand Down Expand Up @@ -1402,13 +1407,16 @@ KD = 2.0E-05 ! [m2 s-1]
! may be used.
KD_MIN = 2.0E-06 ! [m2 s-1] default = 2.0E-07
! The minimum diapycnal diffusivity.
PRANDTL_BKGND = 1.0 ! [nondim] default = 1.0
! Turbulent Prandtl number used to convert vertical
! background diffusivities into viscosities.
BRYAN_LEWIS_DIFFUSIVITY = False ! [Boolean] default = False
! If true, use a Bryan & Lewis (JGR 1979) like tanh
! profile of background diapycnal diffusivity with depth.
! This is done via CVMix.
HORIZ_VARYING_BACKGROUND = False ! [Boolean] default = False
! If true, apply vertically uniform, latitude-dependent background
! diffusivity, as described in Danabasoglu et al., 2012
PRANDTL_BKGND = 1.0 ! [nondim] default = 1.0
! Turbulent Prandtl number used to convert vertical
! background diffusivities into viscosities.
HENYEY_IGW_BACKGROUND = True ! [Boolean] default = False
! If true, use a latitude-dependent scaling for the near
! surface background diffusivity, as described in
Expand Down
14 changes: 11 additions & 3 deletions coupled_AM2_LM3_SIS2/AM2_SIS2_MOM6i_1deg/MOM_parameter_doc.all
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Original file line number Diff line number Diff line change
Expand Up @@ -75,6 +75,11 @@ THERMO_SPANS_COUPLING = False ! [Boolean] default = False
! The actual thermodynamic timestep that is used in this
! case is the largest integer multiple of the coupling
! timestep that is less than or equal to DT_THERM.
HFREEZE = -1.0 ! [m] default = -1.0
! If HFREEZE > 0, melt potential will be computed. The actual depth
! over which melt potential is computed will be min(HFREEZE, OBLD),
! where OBLD is the boundary layer depth. If HFREEZE <= 0 (default),
! melt potential will not be computed.
MIN_Z_DIAG_INTERVAL = 2.16E+04 ! [s] default = 0.0
! The minimum amount of time in seconds between
! calculations of depth-space diagnostics. Making this
Expand Down Expand Up @@ -1398,13 +1403,16 @@ KD = 2.0E-05 ! [m2 s-1]
! may be used.
KD_MIN = 2.0E-06 ! [m2 s-1] default = 2.0E-07
! The minimum diapycnal diffusivity.
PRANDTL_BKGND = 1.0 ! [nondim] default = 1.0
! Turbulent Prandtl number used to convert vertical
! background diffusivities into viscosities.
BRYAN_LEWIS_DIFFUSIVITY = False ! [Boolean] default = False
! If true, use a Bryan & Lewis (JGR 1979) like tanh
! profile of background diapycnal diffusivity with depth.
! This is done via CVMix.
HORIZ_VARYING_BACKGROUND = False ! [Boolean] default = False
! If true, apply vertically uniform, latitude-dependent background
! diffusivity, as described in Danabasoglu et al., 2012
PRANDTL_BKGND = 1.0 ! [nondim] default = 1.0
! Turbulent Prandtl number used to convert vertical
! background diffusivities into viscosities.
HENYEY_IGW_BACKGROUND = True ! [Boolean] default = False
! If true, use a latitude-dependent scaling for the near
! surface background diffusivity, as described in
Expand Down
14 changes: 11 additions & 3 deletions coupled_AM2_LM3_SIS2/Concurrent_ice_1deg/MOM_parameter_doc.all
View file
Original file line number Diff line number Diff line change
Expand Up @@ -75,6 +75,11 @@ THERMO_SPANS_COUPLING = False ! [Boolean] default = False
! The actual thermodynamic timestep that is used in this
! case is the largest integer multiple of the coupling
! timestep that is less than or equal to DT_THERM.
HFREEZE = -1.0 ! [m] default = -1.0
! If HFREEZE > 0, melt potential will be computed. The actual depth
! over which melt potential is computed will be min(HFREEZE, OBLD),
! where OBLD is the boundary layer depth. If HFREEZE <= 0 (default),
! melt potential will not be computed.
MIN_Z_DIAG_INTERVAL = 2.16E+04 ! [s] default = 0.0
! The minimum amount of time in seconds between
! calculations of depth-space diagnostics. Making this
Expand Down Expand Up @@ -1398,13 +1403,16 @@ KD = 2.0E-05 ! [m2 s-1]
! may be used.
KD_MIN = 2.0E-06 ! [m2 s-1] default = 2.0E-07
! The minimum diapycnal diffusivity.
PRANDTL_BKGND = 1.0 ! [nondim] default = 1.0
! Turbulent Prandtl number used to convert vertical
! background diffusivities into viscosities.
BRYAN_LEWIS_DIFFUSIVITY = False ! [Boolean] default = False
! If true, use a Bryan & Lewis (JGR 1979) like tanh
! profile of background diapycnal diffusivity with depth.
! This is done via CVMix.
HORIZ_VARYING_BACKGROUND = False ! [Boolean] default = False
! If true, apply vertically uniform, latitude-dependent background
! diffusivity, as described in Danabasoglu et al., 2012
PRANDTL_BKGND = 1.0 ! [nondim] default = 1.0
! Turbulent Prandtl number used to convert vertical
! background diffusivities into viscosities.
HENYEY_IGW_BACKGROUND = True ! [Boolean] default = False
! If true, use a latitude-dependent scaling for the near
! surface background diffusivity, as described in
Expand Down
14 changes: 11 additions & 3 deletions ice_ocean_SIS2/Baltic/MOM_parameter_doc.all
View file
Original file line number Diff line number Diff line change
Expand Up @@ -75,6 +75,11 @@ THERMO_SPANS_COUPLING = False ! [Boolean] default = False
! The actual thermodynamic timestep that is used in this
! case is the largest integer multiple of the coupling
! timestep that is less than or equal to DT_THERM.
HFREEZE = -1.0 ! [m] default = -1.0
! If HFREEZE > 0, melt potential will be computed. The actual depth
! over which melt potential is computed will be min(HFREEZE, OBLD),
! where OBLD is the boundary layer depth. If HFREEZE <= 0 (default),
! melt potential will not be computed.
MIN_Z_DIAG_INTERVAL = 2.16E+04 ! [s] default = 0.0
! The minimum amount of time in seconds between
! calculations of depth-space diagnostics. Making this
Expand Down Expand Up @@ -1398,13 +1403,16 @@ KD = 2.0E-05 ! [m2 s-1]
! may be used.
KD_MIN = 2.0E-06 ! [m2 s-1] default = 2.0E-07
! The minimum diapycnal diffusivity.
PRANDTL_BKGND = 1.0 ! [nondim] default = 1.0
! Turbulent Prandtl number used to convert vertical
! background diffusivities into viscosities.
BRYAN_LEWIS_DIFFUSIVITY = False ! [Boolean] default = False
! If true, use a Bryan & Lewis (JGR 1979) like tanh
! profile of background diapycnal diffusivity with depth.
! This is done via CVMix.
HORIZ_VARYING_BACKGROUND = False ! [Boolean] default = False
! If true, apply vertically uniform, latitude-dependent background
! diffusivity, as described in Danabasoglu et al., 2012
PRANDTL_BKGND = 1.0 ! [nondim] default = 1.0
! Turbulent Prandtl number used to convert vertical
! background diffusivities into viscosities.
HENYEY_IGW_BACKGROUND = True ! [Boolean] default = False
! If true, use a latitude-dependent scaling for the near
! surface background diffusivity, as described in
Expand Down
14 changes: 11 additions & 3 deletions ice_ocean_SIS2/Baltic_ALE_z_offline_tracers/MOM_parameter_doc.all
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Original file line number Diff line number Diff line change
Expand Up @@ -83,6 +83,11 @@ HMIX_UV_SFC_PROP = 0.0 ! [m] default = 0.0
! If BULKMIXEDLAYER is false, HMIX_UV_SFC_PROP is the depth
! over which to average to find surface flow properties,
! SSU, SSV. A non-positive value indicates no averaging.
HFREEZE = -1.0 ! [m] default = -1.0
! If HFREEZE > 0, melt potential will be computed. The actual depth
! over which melt potential is computed will be min(HFREEZE, OBLD),
! where OBLD is the boundary layer depth. If HFREEZE <= 0 (default),
! melt potential will not be computed.
MIN_Z_DIAG_INTERVAL = 2.16E+04 ! [s] default = 0.0
! The minimum amount of time in seconds between
! calculations of depth-space diagnostics. Making this
Expand Down Expand Up @@ -1612,13 +1617,16 @@ KDML = 2.0E-05 ! [m2 s-1] default = 2.0E-05
! If BULKMIXEDLAYER is false, KDML is the elevated
! diapycnal diffusivity in the topmost HMIX of fluid.
! KDML is only used if BULKMIXEDLAYER is false.
PRANDTL_BKGND = 1.0 ! [nondim] default = 1.0
! Turbulent Prandtl number used to convert vertical
! background diffusivities into viscosities.
BRYAN_LEWIS_DIFFUSIVITY = False ! [Boolean] default = False
! If true, use a Bryan & Lewis (JGR 1979) like tanh
! profile of background diapycnal diffusivity with depth.
! This is done via CVMix.
HORIZ_VARYING_BACKGROUND = False ! [Boolean] default = False
! If true, apply vertically uniform, latitude-dependent background
! diffusivity, as described in Danabasoglu et al., 2012
PRANDTL_BKGND = 1.0 ! [nondim] default = 1.0
! Turbulent Prandtl number used to convert vertical
! background diffusivities into viscosities.
HENYEY_IGW_BACKGROUND = True ! [Boolean] default = False
! If true, use a latitude-dependent scaling for the near
! surface background diffusivity, as described in
Expand Down
14 changes: 11 additions & 3 deletions ice_ocean_SIS2/Baltic_OM4_025/MOM_parameter_doc.all
View file
Original file line number Diff line number Diff line change
Expand Up @@ -83,6 +83,11 @@ HMIX_UV_SFC_PROP = 0.0 ! [m] default = 0.0
! If BULKMIXEDLAYER is false, HMIX_UV_SFC_PROP is the depth
! over which to average to find surface flow properties,
! SSU, SSV. A non-positive value indicates no averaging.
HFREEZE = -1.0 ! [m] default = -1.0
! If HFREEZE > 0, melt potential will be computed. The actual depth
! over which melt potential is computed will be min(HFREEZE, OBLD),
! where OBLD is the boundary layer depth. If HFREEZE <= 0 (default),
! melt potential will not be computed.
MIN_Z_DIAG_INTERVAL = 2.16E+04 ! [s] default = 0.0
! The minimum amount of time in seconds between
! calculations of depth-space diagnostics. Making this
Expand Down Expand Up @@ -1647,13 +1652,16 @@ KDML = 1.5E-05 ! [m2 s-1] default = 1.5E-05
! If BULKMIXEDLAYER is false, KDML is the elevated
! diapycnal diffusivity in the topmost HMIX of fluid.
! KDML is only used if BULKMIXEDLAYER is false.
PRANDTL_BKGND = 1.0 ! [nondim] default = 1.0
! Turbulent Prandtl number used to convert vertical
! background diffusivities into viscosities.
BRYAN_LEWIS_DIFFUSIVITY = False ! [Boolean] default = False
! If true, use a Bryan & Lewis (JGR 1979) like tanh
! profile of background diapycnal diffusivity with depth.
! This is done via CVMix.
HORIZ_VARYING_BACKGROUND = False ! [Boolean] default = False
! If true, apply vertically uniform, latitude-dependent background
! diffusivity, as described in Danabasoglu et al., 2012
PRANDTL_BKGND = 1.0 ! [nondim] default = 1.0
! Turbulent Prandtl number used to convert vertical
! background diffusivities into viscosities.
HENYEY_IGW_BACKGROUND = True ! [Boolean] default = False
! If true, use a latitude-dependent scaling for the near
! surface background diffusivity, as described in
Expand Down
14 changes: 11 additions & 3 deletions ice_ocean_SIS2/Baltic_OM4_05/MOM_parameter_doc.all
View file
Original file line number Diff line number Diff line change
Expand Up @@ -83,6 +83,11 @@ HMIX_UV_SFC_PROP = 0.0 ! [m] default = 0.0
! If BULKMIXEDLAYER is false, HMIX_UV_SFC_PROP is the depth
! over which to average to find surface flow properties,
! SSU, SSV. A non-positive value indicates no averaging.
HFREEZE = -1.0 ! [m] default = -1.0
! If HFREEZE > 0, melt potential will be computed. The actual depth
! over which melt potential is computed will be min(HFREEZE, OBLD),
! where OBLD is the boundary layer depth. If HFREEZE <= 0 (default),
! melt potential will not be computed.
MIN_Z_DIAG_INTERVAL = 2.16E+04 ! [s] default = 0.0
! The minimum amount of time in seconds between
! calculations of depth-space diagnostics. Making this
Expand Down Expand Up @@ -1660,13 +1665,16 @@ KDML = 1.5E-05 ! [m2 s-1] default = 1.5E-05
! If BULKMIXEDLAYER is false, KDML is the elevated
! diapycnal diffusivity in the topmost HMIX of fluid.
! KDML is only used if BULKMIXEDLAYER is false.
PRANDTL_BKGND = 1.0 ! [nondim] default = 1.0
! Turbulent Prandtl number used to convert vertical
! background diffusivities into viscosities.
BRYAN_LEWIS_DIFFUSIVITY = False ! [Boolean] default = False
! If true, use a Bryan & Lewis (JGR 1979) like tanh
! profile of background diapycnal diffusivity with depth.
! This is done via CVMix.
HORIZ_VARYING_BACKGROUND = False ! [Boolean] default = False
! If true, apply vertically uniform, latitude-dependent background
! diffusivity, as described in Danabasoglu et al., 2012
PRANDTL_BKGND = 1.0 ! [nondim] default = 1.0
! Turbulent Prandtl number used to convert vertical
! background diffusivities into viscosities.
HENYEY_IGW_BACKGROUND = True ! [Boolean] default = False
! If true, use a latitude-dependent scaling for the near
! surface background diffusivity, as described in
Expand Down
14 changes: 11 additions & 3 deletions ice_ocean_SIS2/OM4_025/MOM_parameter_doc.all
View file
Original file line number Diff line number Diff line change
Expand Up @@ -83,6 +83,11 @@ HMIX_UV_SFC_PROP = 0.0 ! [m] default = 0.0
! If BULKMIXEDLAYER is false, HMIX_UV_SFC_PROP is the depth
! over which to average to find surface flow properties,
! SSU, SSV. A non-positive value indicates no averaging.
HFREEZE = -1.0 ! [m] default = -1.0
! If HFREEZE > 0, melt potential will be computed. The actual depth
! over which melt potential is computed will be min(HFREEZE, OBLD),
! where OBLD is the boundary layer depth. If HFREEZE <= 0 (default),
! melt potential will not be computed.
MIN_Z_DIAG_INTERVAL = 2.16E+04 ! [s] default = 0.0
! The minimum amount of time in seconds between
! calculations of depth-space diagnostics. Making this
Expand Down Expand Up @@ -1647,13 +1652,16 @@ KDML = 1.5E-05 ! [m2 s-1] default = 1.5E-05
! If BULKMIXEDLAYER is false, KDML is the elevated
! diapycnal diffusivity in the topmost HMIX of fluid.
! KDML is only used if BULKMIXEDLAYER is false.
PRANDTL_BKGND = 1.0 ! [nondim] default = 1.0
! Turbulent Prandtl number used to convert vertical
! background diffusivities into viscosities.
BRYAN_LEWIS_DIFFUSIVITY = False ! [Boolean] default = False
! If true, use a Bryan & Lewis (JGR 1979) like tanh
! profile of background diapycnal diffusivity with depth.
! This is done via CVMix.
HORIZ_VARYING_BACKGROUND = False ! [Boolean] default = False
! If true, apply vertically uniform, latitude-dependent background
! diffusivity, as described in Danabasoglu et al., 2012
PRANDTL_BKGND = 1.0 ! [nondim] default = 1.0
! Turbulent Prandtl number used to convert vertical
! background diffusivities into viscosities.
HENYEY_IGW_BACKGROUND = True ! [Boolean] default = False
! If true, use a latitude-dependent scaling for the near
! surface background diffusivity, as described in
Expand Down
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