[MITgcm-devel] free drift ice model
Dimitris Menemenlis
menemenlis at sbcglobal.net
Wed Nov 29 19:07:18 EST 2006
> Should maybe be a bit careful re. applicability of Arctic numbers
> for Antarctic sea-ice (latter seems more "loose", so more in free drift).
> But maybe ok as first guess.
agree. also differences in roughness. multiyear Arctic ice is much rougher
because of sails and keels than first year Antarctic ice. that is why I
suggested to use 1st year ice numbers. but in most of Arctic first-year ice
areas away from coastlines, internal ice stress are negligible compared to
ice-ocean drag, as is case for Antarctic.
> Maybe again be careful in stating what works when.
> Matt probably still has B-grid code enabled for which
> his assumption is correct.
> But good to hear, the C-grid code has it.
> Might be worth switching then if it's "well" tested. Is it?
you are right. this only works for c-grid. it's tested and it works well, but
not yet "well" tested. will let you know how it goes.
> I ran v3.iter0 with latest growth code.
> Seaice concentration misfits is reduced by 2/3, not bad.
cool! did you turn on sea-ice in adjoint? or is it passive?
> Still unclear re. fin.diff. sensitivities.
> Question is, which part of the code did it.
I will experiment with the snow stuff I discussed in earlier e-mail and let you
know how it goes.
D.
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