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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? |