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A Study on the Nonlinear Stability of Fronts in the Ocean on a Sloping Continental Shelf


doi: 10.1007/s00376-000-0009-6

  • The baroclinic nonlinear stability of fronts in the ocean on a sloping continental shelf is studied, the model equations, called the frontal geostrophic model, developed by Cushman-Roisin et al. (1992) for des-cribing the dynamics of surface density fronts in the ocean are developed and the two-layer frontal geostrophic model for fronts on a sloping continental shelf is first obtained. The nonlinear stability criteria for the fronts on a sloping bottom are obtained by using Arnol'd (1965, 1969) variational principle and a prior estimate method. It is shown that our result is better than the former works.
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Manuscript History

Manuscript received: 10 April 2000
Manuscript revised: 10 April 2000
通讯作者: 陈斌, bchen63@163.com
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A Study on the Nonlinear Stability of Fronts in the Ocean on a Sloping Continental Shelf

  • 1. LASG Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029,LASG Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029,LASG Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029

Abstract: The baroclinic nonlinear stability of fronts in the ocean on a sloping continental shelf is studied, the model equations, called the frontal geostrophic model, developed by Cushman-Roisin et al. (1992) for des-cribing the dynamics of surface density fronts in the ocean are developed and the two-layer frontal geostrophic model for fronts on a sloping continental shelf is first obtained. The nonlinear stability criteria for the fronts on a sloping bottom are obtained by using Arnol'd (1965, 1969) variational principle and a prior estimate method. It is shown that our result is better than the former works.

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