Drifting snow is a complicated and poorly understood
process that is important to fathom because it accounts for a major fraction of wind - blown
snow redistribution within polar and mountainous regions of the world.
These OMITTED / POORLY Represented
processes include the following: oceanic eddies, tides, fronts, buoyancy - driven coastal and boundary currents, cold halocline, dense water plumes and convection, double diffusion, surface / bottom mixed layer, sea ice — thickness distribution, concentration, deformation,
drift and export, fast ice,
snow cover, melt ponds and surface albedo, atmospheric loading, clouds and fronts, ice sheets / caps and mountain glaciers, permafrost, river runoff, and air — sea ice — land interactions and coupling.