Stability of large-amplitude geostrophic flows localized in a thin layer

Author:

Benilov E. S.

Abstract

In this paper the dynamics of geostrophic flows localized in a thin layer of continuously stratified fluid, which overrides a thick homogeneous layer are studied. The displacement of isopycnal surfaces is assumed large; the β-effect is strong, i.e. \[(R_0/R_e)\cot\theta\gtrsim\epsilon, \] where ε is the Rossby number, θ is the latitude; Re is the Earth's radius, and R0 is the deformation radius based on the total depth of the ocean. An asymptotic system of equations is derived and used to study the stability of zonal currents. Three sufficient conditions of stability are obtained, which restrict the slope of the interface between the stratified and non-stratified layers. The results obtained are applied to the subtropical and subarctic frontal currents in the Northern Pacific: the former was found to be stable, the latter was found to be unstable. However, the growth rate of the instability is very small (the effective time of growth is about 2 years).

Publisher

Cambridge University Press (CUP)

Subject

Mechanical Engineering,Mechanics of Materials,Condensed Matter Physics

Reference18 articles.

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2. Benilov, E. S. 1994 Dynamics of large-amplitude geostrophic flows: the case of ‘strong’ beta-effect.J. Fluid Mech. 262,157–169.

3. Odulo, A. B. 1979 Long non-linear waves in the rotating ocean of variable depth.Dokl. Earth Sci. Sect. 248,218–220.

4. Killworth, P. D. 1992 An equivalent-barotropic mode in the Fine Resolution Antarctic Model.J. Phys. Oceanogr. 22,1379–1387.

5. Barcilon, A. & Blumen, W. 1995 The Eady problem with linear horizontal shear.Dyn. Atmos. Oceans (submitted).

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