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Effects of Stochastic Ice Strength Perturbation on Arctic Finite Element Sea Ice Modeling
Publisher: American Meteorological Society
Abstract: he 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 ...
Systematic Errors in Weather and Climate Models: Nature, Origins, and Ways Forward
Publisher: American Meteorological Society
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