Abstract
Presents a three layer model of ocean circulation in a Northern Hemisphere basin driven by winds that are anticyclonic in the south and cyclonic in the north. The model also includes the effects of surface cooling.
Cite
CITATION STYLE
APA
Veronis, G. (1988). Circulation driven by winds and surface cooling. J. PHYS. OCEANOGR., 18(12, Dec. 1988), 1920–1932. https://doi.org/10.1175/1520-0485(1988)018<1920:cdbwas>2.0.co;2
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