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Both horizontal and vertical discretization of the sea ice model is presented
here, as well as category discretization. Two forms of horizontal discretization
are distinguished: a global 2D domain decomposition, and an exclusion of lower
latitude regions of no ice in the exchange with the coupler. The ice thickness
category discretization can be thought of as a horizontal discretization by
ice thickness. The vertical discretization varies with ice thickness category.
Subsections
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