Stationary Vortices of Elliptic Boundary in Drift and Geostrophic Shear Flows
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概要
- 論文の詳細を見る
An analytic solution of' the Charney-Haseg;twa-lVIiuaaa eqtraiton, a two-dirnensional nonlinearequation describing geostrophic Rossby floxv and plasma drift flow, is given which representsa stationary vortex of an elliptic botnndaxry in a background flow having a linear shear, Thesoltrtion is obtained throtrgh an appropriate ansatz for the arbitrary f'tunction of integration of thestationary equation. Three types of' vortices ettaerge according to the chioce of parameters whichcharacterize the distribution of vorticity: a generally asynarnetric dipole inside the boundaryellipse E, a zaaonopole inside E, and a larger dipole lying across E.
- 社団法人日本物理学会の論文
- 1997-05-15
著者
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Sato Masatomo
Department Of Physics And Atomic Energy Research Institute College Of Science And Engineering Nihon
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Kato Yoko
Department Of Materials Science Shizuoka Institute Of Science And Technology
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KOIDE Noriko
Department of Physics,College of Science and Technology,Nihon University
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Kato Yoko
Department Of Biomedical Laboratory Sciences School Of Health Sciences Shinshu University
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Koide Noriko
Department Of Physics College Of Science And Technology Nihon University
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