+*Revise non-Boussinesq offline tracer diffusivity #461
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Rescale the units diapycnal diffusivity used in the offline tracer mode to work in [H Z T-1 ~> m2 s-1 or kg m-1 s-1], making it consistent with what has already been done for other diapycnal diffusivities. This change involves changes to the units of arguments to update_offline_from_files and ALE_offline_inputs and to two elements of offline_transport_CS. It also includes a new thermo_vary_type argument to offline_diabatic_ale, as well as a call to thickness_to_dz in that same routine to set the values of the newly added 3-d array of the vertical distances across layers and a change in name and units of the inverse thickness variable used to find the fluxes. All answers are bitwise identical in Boussinesq mode, but in offline tracer calculations in non-Boussinesq mode they will change to become independent of the Boussinesq reference density.
Codecov Report
@@ Coverage Diff @@
## dev/gfdl #461 +/- ##
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Coverage 38.01% 38.01%
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Files 270 270
Lines 77761 77763 +2
Branches 14371 14371
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+ Hits 29558 29560 +2
Misses 42837 42837
Partials 5366 5366
... and 1 file with indirect coverage changes 📣 We’re building smart automated test selection to slash your CI/CD build times. Learn more |
marshallward
approved these changes
Aug 30, 2023
|
Gaea regression: https://gitlab.gfdl.noaa.gov/ogrp/MOM6/-/pipelines/20491 ✔️ |
This was referenced Nov 13, 2023
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Rescale the units diapycnal diffusivity used in the offline tracer mode to work in [H Z T-1 ~> m2 s-1 or kg m-1 s-1], making it consistent with what has already been done for other diapycnal diffusivities. This change involves changes to the units of arguments to update_offline_from_files and ALE_offline_inputs and to two elements of offline_transport_CS. It also includes a new thermo_vary_type argument to offline_diabatic_ale, as well as a call to thickness_to_dz in that same routine to set the values of the newly added 3-d array of the vertical distances across layers and a change in name and units of the inverse thickness variable used to find the fluxes. All answers are bitwise identical in Boussinesq mode, but in offline tracer calculations in non-Boussinesq mode they will change to become independent of the Boussinesq reference density.