Currently the atm->ice mapping (almost) follows CM2:
CICE exports ice fractions to UM (fraction of non-land area covered by sea ice) with first order conservative remapping (
UM: divide fluxes (averaged over non-land area) by ice area fraction (local ice fluxes)3.
First order conservative remapping to CICE grid
This almost conserves energy, but does not take into account changes in the ice fraction over subsequent CICE time steps.
TODO: scale fluxes by initial ice area / current ice area to maintain energy conservation. This has caused numerical instabilities in the past - revisit in the future when things are more stable.
Currently the atm->ice mapping (almost) follows CM2:
This almost conserves energy, but does not take into account changes in the ice fraction over subsequent CICE time steps.
TODO: scale fluxes by
initial ice area / current ice area
to maintain energy conservation. This has caused numerical instabilities in the past - revisit in the future when things are more stable.