Finite depth stratified flow over topography on a beta-plane
作者:
E.R. Johnson,
期刊:
Geophysical & Astrophysical Fluid Dynamics
(Taylor Available online 1979)
卷期:
Volume 12,
issue 1
页码: 35-43
ISSN:0309-1929
年代: 1979
DOI:10.1080/03091927908242675
出版商: Taylor & Francis Group
数据来源: Taylor
摘要:
The form of quasi-geostrophic flow past isolated topography on a beta plane is obtained for finite depth, linearly stratified flow. The response is shown to consist of an isotropic perturbation plus, in eastward flows, a single barotropic and a finite number of baroclinic waves. The form of the solution allows a rapid calculation of the Rossby wave drag on an axisymmetric obstacle in an eastward flow.
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