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@gustavo-marques gustavo-marques commented Jan 8, 2025

  • Adds new topographic edits and updated channel list. These lead to slightly improved circulation and hydrograph (Response to bathymetry edits NCAR/omwg_dev#55)
  • Enabled COMPUTE_MONIN_OBUKHOV = True to improve the OBL seasonal cycle by limiting the OBL depth to no deeper than the Monin-Obukhov depth. Because of this change, we now need to assure that OBL is always >= than the first thickness (dz) used in the model. This is done by setting MINIMUM_OBL_DEPTH = 2.5.
  • Updated background mixing parameters:
    • KV = 1.0E-06
    • KD = 1.0E-07
    • PRANDTL_BKGND = 10
  • Enable bug fixes introduced in GFDL to main (2024-11-27) mom-ocean/MOM6#1647

Fixes: #218, #213, #208, #220

- Added new topographic edits and updated channel list.
- Enabled COMPUTE_MONIN_OBUKHOV = True to improve the OBL seasonal cycle by limiting the OBL depth to no deeper than the Monin-Obukhov depth.
- Updated background mixing parameters:
  - KV = 1.0E-6
  - KD = 1.0E-7
  - PRANDTL_BKGND = 10
- Configured MLE backup settings:
  - Set MLE_FRONT_LENGTH_FROM_FILE = True
  - Updated MLE_FL_FILE to "mle-lf-clim-tx2_3v2_20250108.nc"
- Enabled Leithy parameterization with:
  - USE_LEITHY = True
  - LEITH_BI_CONST = 90.0
  - LEITHY_CK = 1.0 (full backscatter)
  - LEITH_AH = False
@gustavo-marques
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I will add the new files to input_data_list.yaml later today.

@gustavo-marques
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I've added MINIMUM_OBL_DEPTH = 2.5 for cases using tx2_3v2. This solves the issue with the GNU debug test reported in NCAR/MOM6#331

@alperaltuntas
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Thanks, @gustavo-marques. I'll re-run the test suite.

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Dimensional scaling test for the L dimension fails when this PR gets merged. I am investigating.

@alperaltuntas
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@gustavo-marques Is this ready for testing now?

@gustavo-marques
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Yes, thanks!

@gustavo-marques
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With the latest beta05 update, we are getting negative Laplacian viscosities near coastlines. @iangrooms thinks this is a bug; fixing it will take a few days (perhaps more). To avoid additional delays in tag creation, we suggest going back to LEITH_AH.

I am also reverting to using a constant frontal length scale for MLE. As Gokhan pointed out yesterday, the MLE overturning with the variable frontal scale is too strong, reverting the near-surface residual MOC in the Southern Ocean (see plot below).
For now, including this in the tag does not make sense.

image

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I updated the initial description by removing the following:

  • Configured MLE settings (this relies on PR #331):
    • Set MLE_FRONT_LENGTH_FROM_FILE = True
    • Updated MLE_FL_FILE to "mle-lf-clim-tx2_3v2_20250115.nc"
  • Enabled Leithy parameterization with:
    • USE_LEITHY = True
    • LEITH_BI_CONST = 90.0
    • LEITHY_CK = 1.0 (full backscatter)
    • LEITH_AH = False

@alperaltuntas alperaltuntas merged commit 70a0af7 into ESCOMP:main Jan 25, 2025
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Add option to specify MLE fronal-length scale via file

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