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Similarly to surface and atmosphere models for the top boundary, PISM should have shelf base and ocean models (instead of one "ocean" lumping ocean forcing with parameterizations of sub-shelf melt).
Rationale:atmosphere models make it relatively easy to modify inputs of a top-surface-process model (using scalar offsets, for example). Currently ocean modifiers allow adjusting outputs of a selected ocean model, but not its inputs.
We would like to be able to use scalar offsets to modify the potential temperature of seawater used as an input of the -ocean th model, for example.
The text was updated successfully, but these errors were encountered:
Similarly to surface and atmosphere models for the top boundary, PISM should have shelf base and ocean models (instead of one "ocean" lumping ocean forcing with parameterizations of sub-shelf melt).
Rationale: atmosphere models make it relatively easy to modify inputs of a top-surface-process model (using scalar offsets, for example). Currently ocean modifiers allow adjusting outputs of a selected ocean model, but not its inputs.
We would like to be able to use scalar offsets to modify the potential temperature of seawater used as an input of the
-ocean th
model, for example.The text was updated successfully, but these errors were encountered: