Effects of convection instability due to incompatibility between ocean dynamics and surface forcings

The study demonstrates that an incompatibility between a surface temperature climatology and a given ocean model, into which the climatology is assimilated via Haney restoration, can cause model ocean climate drift and interdecadal oscillations when the ocean is switched to a weaker restoration....

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Bibliographic Details
Main Authors: W. Cai, P. C. Chu
Format: Article
Language:English
Published: Copernicus Publications 1997-08-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/15/1067/1997/angeo-15-1067-1997.pdf