Abstract
The flow from a line source to a line sink in a multiply connected region is discussed. It is shown that the transport from source to sink passes through the interior region and the Stewartson layers as well as through the Ekman layers.
Publisher
Cambridge University Press (CUP)
Cited by
7 articles.
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1. Spin-up of a source-sink flow over a model continental shelf;Geophysical & Astrophysical Fluid Dynamics;1998-09
2. On asymmetry in Stewartson layers;Journal of Engineering Mathematics;1990-02
3. Fluid flow in a partially-filled rotating cylinder;Journal of Engineering Mathematics;1986-09
4. Source-sink flow in a rotating cylinder;Journal of Engineering Mathematics;1984-09
5. Frontal upwelling in a rotating two-layer fluid;Geophysical & Astrophysical Fluid Dynamics;1984-05