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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Autori principali: Lionel Renault, S. Masson, T. Arsouze, Gurvan Madec, James C. McWilliams
Natura: Artigo
Lingua:Inglês
Pubblicazione: American Geophysical Union (AGU) 2020-02-01
Serie:Journal of Advances in Modeling Earth Systems
Soggetti:
Air‐Sea interaction
Current Feedback
Parameterization
Forced Ocean Model
Reanalysis
Scatterometers
Accesso online:https://doi.org/10.1029/2019MS001715
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