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On the problem of the formation of the Greenland sea convective gyre |
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| Authors: | P V Bogorodsky A V Marchenko I A Podgorny |
| Abstract: | The transformation of the interfaces of a rotating three-layer fluid is described through a simple hydrodynamic model using the shallow-water approximation. Using the Greenland sea gyre as an example, it is shown that a cyclonic circulation results in the oncoming deflection of the upper and lower layers, which favours the development of deep convection.Translated by Mikhail M. Trufanov. |
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