CHISLENNAYA MODEL' BAROKLINNOI NEUSTOICHIVOSTI OSESIMMETRICHNYKH VIKHREI V KVUKHSLOINOM OKEANE.

V. F. Kozlov; V. G. Makarov; M. A. Sokolovsky

CHISLENNAYA MODEL' BAROKLINNOI NEUSTOICHIVOSTI OSESIMMETRICHNYKH VIKHREI V KVUKHSLOINOM OKEANE.

V. F. Kozlov, V. G. Makarov, M. A. Sokolovsky

Centro Interdisciplinario de Ciencias Marinas (CICIMAR)

Producción científica: Contribución a una revista › Artículo › revisión exhaustiva

17 Citas (Scopus)

Resumen

A numerical quasi-geostrophic model of the evolution of vortical perturbations in a two-layer ocean is proposed which is based on the use of the contour-dynamics method. A detailed study is made of the case of an axisymmetric vortex on the OMEGA -plane. A numerical experiment performed confirms the conclusions of a linear stability analysis and makes it possible to follow the nonlinear stage of evolution of a system disintegrating into two vortices with inclined axes spreading in opposite directions.

Título traducido de la contribución	Numerical Model of Baroclinic Instability of Axisymmetric Vortices in a Two-Layer Ocean.
Idioma original	Ruso
Páginas (desde-hasta)	868-874
Número de páginas	7
Publicación	Izvestia Akademii nauk SSSR. Fizika atmosfery i okeana
Volumen	22
N.º	8
Estado	Publicada - ago. 1986

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abstract = "A numerical quasi-geostrophic model of the evolution of vortical perturbations in a two-layer ocean is proposed which is based on the use of the contour-dynamics method. A detailed study is made of the case of an axisymmetric vortex on the OMEGA -plane. A numerical experiment performed confirms the conclusions of a linear stability analysis and makes it possible to follow the nonlinear stage of evolution of a system disintegrating into two vortices with inclined axes spreading in opposite directions.",

author = "Kozlov, {V. F.} and Makarov, {V. G.} and Sokolovsky, {M. A.}",

year = "1986",

month = aug,

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AU - Makarov, V. G.

AU - Sokolovsky, M. A.

PY - 1986/8

Y1 - 1986/8

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AB - A numerical quasi-geostrophic model of the evolution of vortical perturbations in a two-layer ocean is proposed which is based on the use of the contour-dynamics method. A detailed study is made of the case of an axisymmetric vortex on the OMEGA -plane. A numerical experiment performed confirms the conclusions of a linear stability analysis and makes it possible to follow the nonlinear stage of evolution of a system disintegrating into two vortices with inclined axes spreading in opposite directions.

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M3 - Artículo

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JF - Izvestia Akademii nauk SSSR. Fizika atmosfery i okeana

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ER -

CHISLENNAYA MODEL' BAROKLINNOI NEUSTOICHIVOSTI OSESIMMETRICHNYKH VIKHREI V KVUKHSLOINOM OKEANE.

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