Calculation of wind currents in the edge zone of a sea ice sheet (Q1317794)
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scientific article; zbMATH DE number 536798
| Language | Label | Description | Also known as |
|---|---|---|---|
| English | Calculation of wind currents in the edge zone of a sea ice sheet |
scientific article; zbMATH DE number 536798 |
Statements
Calculation of wind currents in the edge zone of a sea ice sheet (English)
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12 April 1994
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The steady wind currents in the ocean new the edge of an ice sheet simulated by a rigid cover are studied. Taking the Coriolis force into account leads to the formation of a spiral flow structure in the vertical direction. The boundary conditions on the surface have a discontinuity at the point corresponding to the edge of the ice; therefore the Wiener-Hopf method is used to construct an analytic solution of the problem.
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linearized Navier-Stokes equations
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Coriolis force
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spiral flow structure
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Wiener-Hopf method
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analytic solution
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0.8383633
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0.8111612
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0.80741507
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0.80653524
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0.80635166
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0.8061983
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0.80605066
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0.8013078
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