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Recipes for How to Force Oceanic Model Dynamics

Abstract The current feedback to the atmosphere (CFB) contributes to the oceanic circulation by damping eddies. In an ocean‐atmosphere coupled model, CFB can be correctly accounted for by using the wind relative to the oceanic current. However, its implementation in a forced oceanic model is less st...

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Detalles Bibliográficos
Main Authors: Lionel Renault, S. Masson, T. Arsouze, Gurvan Madec, James C. McWilliams
Formato: Artigo
Idioma:Inglês
Publicado: American Geophysical Union (AGU) 2020-02-01
Series:Journal of Advances in Modeling Earth Systems
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Acceso en liña:https://doi.org/10.1029/2019MS001715
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