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In the 1-deg MOM6 configuration, there is no land at the southern boundary (j=1). Since CICE6 obtains its land mask from the MOM6 configuration, CICE6 currently has no land at j=1 either.
MOM6 utilizes a C-grid while CICE6 utilizes the B-grid. During testing by the hygrid-godas team running the 1-deg configuration with the DATM, locations of very thick ice were seen developing in isolated single point locations.
Information provided by @apcraig addresses both these issues:
The open boundary at j=1 is going to be problematic in the long term as the CICE6 ns_boundary_type='tripole' which means it's using "open" on the southern boundary.
The thick ice seen in hybrid-godas configuration appear to be related to isolated ocean points. In other words, they are connected to only 1 other active gridcell. In pop, this was always a no-no because there could be no velocity in a gridcell that was isolated like that. I don't know what the restrictions are on MOM, but my guess is that the thick ice is related to this choice of masking. Because of the pop constraint, I don't have any experience running CICE with isolated cells like this. But the problem is that in a B-grid, you probably will not get any velocity at that cell.
The text was updated successfully, but these errors were encountered:
In the 1-deg MOM6 configuration, there is no land at the southern boundary (j=1). Since CICE6 obtains its land mask from the MOM6 configuration, CICE6 currently has no land at j=1 either.
MOM6 utilizes a C-grid while CICE6 utilizes the B-grid. During testing by the hygrid-godas team running the 1-deg configuration with the DATM, locations of very thick ice were seen developing in isolated single point locations.
Information provided by @apcraig addresses both these issues:
The open boundary at j=1 is going to be problematic in the long term as the CICE6 ns_boundary_type='tripole' which means it's using "open" on the southern boundary.
The thick ice seen in hybrid-godas configuration appear to be related to isolated ocean points. In other words, they are connected to only 1 other active gridcell. In pop, this was always a no-no because there could be no velocity in a gridcell that was isolated like that. I don't know what the restrictions are on MOM, but my guess is that the thick ice is related to this choice of masking. Because of the pop constraint, I don't have any experience running CICE with isolated cells like this. But the problem is that in a B-grid, you probably will not get any velocity at that cell.
The text was updated successfully, but these errors were encountered: