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(*) Bugfix: [uv]hml z-diags in general restrat#985

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adcroft merged 1 commit intomom-ocean:dev/gfdlfrom
marshallward:uhml_bugfix_general
Aug 30, 2019
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(*) Bugfix: [uv]hml z-diags in general restrat#985
adcroft merged 1 commit intomom-ocean:dev/gfdlfrom
marshallward:uhml_bugfix_general

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The z-interpolated uhml and vhml diagnostics gave inconsistent answers
across layouts when using the general mixed layer restratification
scheme, because the value of h had changed but its halos had not been
updated.

This had been previously fixed in the BML restratification but not the
general stratification method.

This patch updates the value of h by conditionally updating the halos if
this diagnostic is required.

The z-interpolated uhml and vhml diagnostics gave inconsistent answers
across layouts when using the general mixed layer restratification
scheme, because the value of h had changed but its halos had not been
updated.

This had been previously fixed in the BML restratification but not the
general stratification method.

This patch updates the value of h by conditionally updating the halos if
this diagnostic is required.
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@adcroft adcroft merged commit f40e692 into mom-ocean:dev/gfdl Aug 30, 2019
@marshallward marshallward deleted the uhml_bugfix_general branch September 3, 2019 15:45
OlgaSergienko pushed a commit to OlgaSergienko/MOM6 that referenced this pull request Dec 2, 2025
* Added frazil to ice shelf

The frazil mass flux to the ice-shelf base is calculated by
multiplying frazil energy [J m-2] by the inverse of the timestep times
the latent heat of fusion [kg J-1 s-1].

This frazil mass flux is incorporated as a negative water flux from
the ice shelf. This negative water flux then acts to add the frazil
mass to the ice shelf base
(MOM_ice_shelf.F90/change_thickness_using_melt) and remove it from
the ocean surface as evaporation (MOM_ice_shelf.F90/add_shelf_flux).

Note frazil is reset to zero at the start of each therm timestep in
MOM.F90/step_MOM.

Some additional changes were also made to how the ice-shelf flux
factor is implemented, so that is only scales ice-shelf melt without
affecting the frazil mass flux.

* Fixed a commented line where fluxes%water_flux should be ISS%water_flux
claireyung pushed a commit to ACCESS-NRI/MOM6 that referenced this pull request Dec 17, 2025
* Added frazil to ice shelf

The frazil mass flux to the ice-shelf base is calculated by
multiplying frazil energy [J m-2] by the inverse of the timestep times
the latent heat of fusion [kg J-1 s-1].

This frazil mass flux is incorporated as a negative water flux from
the ice shelf. This negative water flux then acts to add the frazil
mass to the ice shelf base
(MOM_ice_shelf.F90/change_thickness_using_melt) and remove it from
the ocean surface as evaporation (MOM_ice_shelf.F90/add_shelf_flux).

Note frazil is reset to zero at the start of each therm timestep in
MOM.F90/step_MOM.

Some additional changes were also made to how the ice-shelf flux
factor is implemented, so that is only scales ice-shelf melt without
affecting the frazil mass flux.

* Fixed a commented line where fluxes%water_flux should be ISS%water_flux
claireyung added a commit to ACCESS-NRI/MOM6 that referenced this pull request Dec 17, 2025
Hallberg-NOAA added a commit to Hallberg-NOAA/MOM6 that referenced this pull request Jan 4, 2026
  Added a test to only apply frazil at the base of an ice shelf if the frazil
array is allocated, thereby avoiding a segmentation fault in cases that have and
ice shelf but do not have the runtime parameter FRAZIL set to true.  This bug
was causing the ocean_only/ISOMIP test cases to fail, and fixing it allows them
to work again, providing the same answers as previously.

  This bug was introduced on Dec. 2, 2025 as a part of PR mom-ocean#985 to dev/gfdl.
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2 participants