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dimitri |
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\section{Discussion and conclusion} |
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\label{sec:concl} |
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The story of the paper could be: |
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B-grid ice model + C-grid ocean model does not work properly for us, |
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therefore C-grid ice model with advantages: |
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\begin{enumerate} |
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\item stress coupling simpler (no interpolation required) |
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\item different boundary conditions |
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\item advection schemes carry over trivially from main code |
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\end{enumerate} |
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LSR/EVP solutions are similar with appropriate bcs, evp parameters as |
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a function of forcing time scale (when does VP solution break |
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down). Same for LSR solver, provided that it works (o: |
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Which scheme is more efficient for the resolution/time stepping |
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parameters that we use here. What about other resolutions? |