Rossby Wave Propagation and Nonlinear Effects in Zonally-Varying Basic Flows
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- Naoe Hiroaki
- Meteorological Research Institute
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- Matsuda Yoshihisa
- Graduate School of Science, University of Tokyo
Bibliographic Information
- Other Title
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- 東西非一様流におけるロスビー波の伝播と非線形効果
- Rossby Wave Propagation and Nonlinear E
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Description
In this study, we examine the nonlinear effect in the evolution of the Rossby wave propagating in the jet stream using a nonlinear barotropic model. We focus primarily on the formation of isolated eddy from the Rossby wave. The Rossby wave is induced by localized vorticity forcing in a zonally-varying basic flow.<br>For weak, steady forcing we obtain the Rossby wavetrain trapped in the jet stream, as in the linear model. For strong, steady forcing it is occasionally seen that an isolated eddy with negative vorticity is formed from some domain in the Rossby wavetrain, when the zonal asymmetry of the basic flow is large. For strong forcing of a finite period, a strong isolated eddy with negative vorticity can be formed from some domain when the zonal asymmetry of basic flow is large. This eddy breaks down to finally emanate Rossby wave downward.
Journal
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- Journal of the Meteorological Society of Japan. Ser. II
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Journal of the Meteorological Society of Japan. Ser. II 76 (3), 385-402, 1998
Meteorological Society of Japan
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Details 詳細情報について
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- CRID
- 1390001206506008320
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- NII Article ID
- 110001807463
- 130007346980
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- NII Book ID
- AN00317933
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- ISSN
- 21869057
- 00261165
- http://id.crossref.org/issn/00261165
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- NDL BIB ID
- 4510901
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- Data Source
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- JaLC
- NDL Search
- Crossref
- NDL Digital Collections (NII-ELS)
- CiNii Articles
- OpenAIRE
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- Abstract License Flag
- Disallowed