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| Paper IPM / M / 2363 |
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| Abstract: | |||||
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In this paper we consider the two dimensional Barotropic-Vorticity
equation in the first quadrant and using a rearrangement
variational principle prove it has a solution. The solution
represents a steady localized topographic ideal flow. The data
given are the behaviour of the flow at infinity, the rearrangement
class of the vorticity field and the height of the localized
seamount.
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