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- convert potential temperature into in-situ temperature. This changes the isomip tests => update tests
- rearrange computation of tLoc, sLoc, pLoc to make code more efficient
- sort out freshwater flux; convert freshwater fluxes to mass fluxes (kg/m^2/s), does not break tests, because in verification/isomip, rhoConstFresh=rhoConst (by accident)
clean up recent check-in with too comments only meant for myself
how embarrassing: total mixup of ice and sea water densities is resolved
clean up a little
add option for convservative form of Hellmer&Olbers (1989) thermodynamics - requires a little reorganization, which affects the testreport results of isomip.htd (only 7 digits of cg2d agree) => update experiment The results are extremely sensitive to details of the algorithm (e.g., order in which sums and differences are taken, etc) so that replacing a term with a (theoretically) exactly equal other term causes the big difference; possibly, because the solution of a quadratic equation is involed. I am not happy about this, but the present formulation appears to be a little more robust. - add a few comments
Change EmPmR units: from m/s to kg/m2/s
replace "recip_rhoConst*horiVertRatio" by mass2rUnit and "rhoConst*recip_horiVertRatio" by rUnit2mass
add a few diagnostics
add a simple boundary layer scheme to reduce noise, off by default for now
replace a '<' by a '.LT.'
- add more sophisticated thermodynamics of Hellmer (1989), this is now the default - give a few constants more intuitive names
- separate shelfice load anomaly from pload (breaks with time dependent forcing), => introduce constant field shelficeLoadAnomaly. Its default is 0., but it may be computed more cleverly from (unknown) t- and s-profiles (tRef, sRef) and actual EOS. For now this has to be done offline. A good approximation of the pressure load anomaly is necessary to avoid large initial adjustment processes underneath deep-reaching shelfice. - small fix in shelfice_thermodynamics
o add new package shelfice
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