Effects of stochastic ice strength perturbation on Arctic finite element sea ice modeling
The ice strength parameter P* is a key parameter in dynamic/thermodynamic sea ice models that cannot be measured directly. Stochastically perturbing P* in the Finite Element Sea Ice–Ocean Model (FESOM) of the Alfred Wegener Institute aims at investigating the effect of uncertainty pertaining to this...
| Main Authors: | , , , |
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| Format: | Journal article |
| Published: |
American Meteorological Society
2013
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