After the slab ocean component computes
the atmosphere-ocean heat fluxes and
updates and
, the
thermodynamic sea ice model takes the latter two variables as input
and computes the atmosphere-ice and ocean-ice
heat fluxes and advances the
state of the sea ice, including
snow depth, surface temperature, ice thickness, ice
fractional coverage, and internal energy profile in the ice.
The physics of the sea ice component model in CAM 3.0 are
discussed in detail in the next chapter.