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