Non-Linear Behaviors of Forced Baroclinic Wave in a Continuous Zonal Flow
Author:
Affiliation:
1. Department of Physics, Faculty of Scicnce, Kyushu University
Publisher
Meteorological Society of Japan
Subject
Atmospheric Science
Link
https://www.jstage.jst.go.jp/article/jmsj1965/62/6/62_6_809/_pdf
Reference24 articles.
1. Barcilon, V. 1964: Role of the Ekman layers in the stability of the symmetric regime obtained in a rotating annulus. J. Atoms. Soc., 21, 291-299.
2. Blumsack, S. L. and P. J. Gierash 1972: Mars: The effects of topography on baroclinic instability. J. Atomos. Sci., 29, 1081-1089.
3. Charny, J. G. and J. G. DeVore, 1979: Multiple flow equilibria in the atmosphere and blocking. J. Atoms. Sci., 36, 1205-1216.
4. Charny, J. G., and D. M. Straus 1980: Form-drag instability, multiple equilibria and propagating planetary waves in baroclinic, orographically forced, planetary systems. J. Atoms. Sci., 37, 1157-1176.
5. Drazin, P. G. 1972: Nonlinear baroclinic instability of a continuous zonal flow of viscous fluid. J. Fluid. Mech., 55, 577-587.
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1. Stratospheric Multiple Equilibria and Seasonal Variations;Journal of the Meteorological Society of Japan. Ser. II;1987
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