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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Bibliographic Details
Main Authors: Lionel Renault, S. Masson, T. Arsouze, Gurvan Madec, James C. McWilliams
Format: Artigo
Language:Inglês
Published: American Geophysical Union (AGU) 2020-02-01
Series:Journal of Advances in Modeling Earth Systems
Subjects:
Air‐Sea interaction
Current Feedback
Parameterization
Forced Ocean Model
Reanalysis
Scatterometers
Online Access:https://doi.org/10.1029/2019MS001715
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