Background currents in the Sea of Japan (a two-layer quasi-geostrophic model)

V. F. Kozlov, V. G. Makarov

Producción científica: Contribución a una revistaArtículorevisión exhaustiva

2 Citas (Scopus)

Resumen

The concept of a background current, which was used earlier for calculation of the barotropic circulation in the Sea of Japan, is generalized for the case of a two-layer fluid in a quasi-geostrophic approach. The account of baroclinity has lead to notable reduction of the stream function amplitudes and allowed the reproduction of most of the qualitative peculiarities of the horizontal structure of the Tsushima current.

Idioma originalInglés
Páginas (desde-hasta)453-457
Número de páginas5
PublicaciónOceanology
Volumen36
N.º4
EstadoPublicada - 1996
Publicado de forma externa

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