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Barotropic flow over finite isolated topography: steady solutions on the beta-plane and the initial value problem

Published online by Cambridge University Press:  26 April 2006

Luanne Thompson  and
Glenn R. Flierl
Luanne Thompson
Affiliation:
School of Oceanography WB-10, University of Washington, Seattle, WA 98195, USA
Glenn R. Flierl
Affiliation:
Massachussetts Institute of Technology, 54-1426, Cambridge, MA 02139, USA
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Abstract

Solutions for inviscid rotating flow over a right circular cylinder of finite height are studied, and comparisons are made to quasi-geostrophic solutions. To study the combined effects of finite topography and the variation of the Coriolis parameter with latitude a steady inviscid model is used. The analytical solution consists of one part which is similar to the quasi-geostrophic solution that is driven by the potential vorticity anomaly over the topography, and another, similar to the solution of potential flow around a cylinder, that is driven by the matching conditions on the edge of the topography. When the characteristic Rossby wave speed is much larger than the background flow velocity, the transport over the topography is enhanced as the streamlines follow lines of constant background potential vorticity. For eastward flow, the Rossby wave drag can be very much larger than that predicted by quasi-geostrophic theory. The combined effects of finite height topography and time-dependence are studied in the inviscid initial value problem on the f-plane using the method of contour dynamics. The method is modified to handle finite topography. When the topography takes up most of the layer depth, a stable oscillation exists with all of the fluid which originates over the topography rotating around the topography. When the Rossby number is order one, a steady trapped vortex solution similar to the one described by Johnson (1978) may be reached.

Type
Research Article
Information
Journal of Fluid Mechanics , Volume 250 , May 1993 , pp. 553 - 586
Copyright
© 1993 Cambridge University Press

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