Contribution of buoyancy fluxes to tropical Pacific sea level variability

<p>Regional anomalies of steric sea level are either due to redistribution of heat and freshwater anomalies or due to ocean–atmosphere buoyancy fluxes. Interannual to decadal variability in sea level across the tropical Pacific is mainly due to steric variations driven by wind stress anomalies...

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Bibliographic Details
Main Authors: P. Wagner, M. Scheinert, C. W. Böning
Format: Article
Language:English
Published: Copernicus Publications 2021-08-01
Series:Ocean Science
Online Access:https://os.copernicus.org/articles/17/1103/2021/os-17-1103-2021.pdf