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A note on the temporal evolution of taylor columns over topography
Authors:GR Bigg
Institution:Department of Applied Mathematics, University of Adelaide, Adelaide, South Australia Australia
Abstract:The formation of two regions of vorticity, one cyclonic and one anticyclonic, after the initiation of flow is discussed. In particular, the linearized case of elongated topography is examined. The non-linear interaction of the two vortices, once formed, is discussed using a simple model.
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