Skip to main content
Log in

Disturbance evolution and the nonlinear stability to the basic flows for two-dimensional quasi-geostrophic motion

  • Papers
  • Published:
Chinese Science Bulletin

Abstract

The status of disturbances of both initial values and parameters in the models is further investigated, the exact explicit estimates on the disturbance energy and disturbance potential enstrophy are given; and while the initial disturbance fields rely only on the initial disturbance potential enstrophy, initial disturbance velocity circulation along the boundary, disturbance parameters, and the nonlinear stability criteria paralleling to Arnold’s second theorem are obtained, and the main results of Mu are generalized.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  1. Pedlosky, J.,Geophysical Fluid Dynamics, New York: Springer-Verlag, 1979.

    Google Scholar 

  2. Arnold, V. I., On an a priori estimate in the theory of hydrodynamical stability,Izv. Uchebn. Zaved. Matematika(English transl.:Amer. Math. Soc. Transl., 1969, 79: 267, 1966, 54: 3.

    Google Scholar 

  3. Mu Mu, Shepherd, T. G., On Arnold ’s second nonlinear stability theorem for two-dimensional quasigeotrophic flow,Geophys. Astrophys. Fluid Dyn., 1994, 75: 21.

    Article  Google Scholar 

  4. Mu Mu, Nonlinear stability of two-dimensional quasi-geostrophic motions,Geophys. Astrophys. Fluid. Dynam., 1992, 65: 57.

    Article  Google Scholar 

  5. Mu Mu, Xiang Jie, On the evolution of finite-amplitude disturbance to the barotropic and baroclinic quasigeostrophic flows,Advances in Atmospheric Sciences, 1998, 11: 3.

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

About this article

Cite this article

Song, S., Liu, Q. Disturbance evolution and the nonlinear stability to the basic flows for two-dimensional quasi-geostrophic motion. Chin.Sci.Bull. 44, 1179–1184 (1999). https://doi.org/10.1007/BF02885960

Download citation

  • Received:

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF02885960

Keywords

Navigation