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Salinity anomaly is very close to the seamount. Unlike the sigma_shelf_zstar case I was trying with triangular ice shelf, it is only very close to the vanishing layers (probably due to the high res, note only 5th layer interface shown below, and the zstar coordinate), and therefore velocities get damped out quickly unlike my triangular ice shelf, leading to lower velocities.
The text was updated successfully, but these errors were encountered:
The salinity anomaly still persists with non-Boussinesq ice shelf. See this notebook https://github.com/pedrocol/MOM6_pge_tests/blob/claire/notebooks/Plot_IC.ipynb
Salinity anomaly is very close to the seamount. Unlike the
sigma_shelf_zstar
case I was trying with triangular ice shelf, it is only very close to the vanishing layers (probably due to the high res, note only 5th layer interface shown below, and the zstar coordinate), and therefore velocities get damped out quickly unlike my triangular ice shelf, leading to lower velocities.The text was updated successfully, but these errors were encountered: