Winter
 (February 15) current velocity
 for
 the HYCOM KPP case in the
 uppermost
 model layer (top) and
 vertically
 averaged within the
 mixed
 layer.
 
 The
 differences show the dominance
 of
 wind-driven ageostrophic flow in
 the
 model surface layer (upper 10m).
 Vertical
 current structure within the
 mixed
 layer could not be resolved by
 MICOM.