Abstract
In order to consider the effect of different ice conditions on the momentum exchange between atmosphere and ocean, a parameterization for variable drag coefficients is introduced. A square dependence on ice concentration is combined with a linear dependence on deformation energy to account for the influence of floe edges as well as for roughness elements in regions with a more compact ice cover. The approach is not regionally specified and is applied over the whole model region. Empirical parameters are optimized via comparison with observed buoy-drift data.
Cite
CITATION STYLE
Steiner, N. (2001). Introduction of variable drag coefficients into sea-ice models. Annals of Glaciology, 33, 181–186. https://doi.org/10.3189/172756401781818149
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