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Vertically, sea ice is discretized into
evenly spaced layers, where the
number of layers of ice (
) depends on the thickness category, with the thinnest
two categories having two equally spaced layers and the thicker three categories
having four. The total sum of vertical levels for all categories is specified in
module
as
, with the maximum number of levels for any
category being
. Several state variables are dependent on vertical level,
as seen in module
.
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