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| Content Provider | Society for Industrial and Applied Mathematics (SIAM) |
|---|---|
| Author | Dalibard, Anne-Laure |
| Copyright Year | 2009 |
| Abstract | The goal of this paper is to describe in mathematical terms the effect on ocean circulation of a random stationary wind stress on the surface of the ocean. In order to avoid singular behavior, nonresonance hypotheses are introduced, which ensure that the time frequencies of the wind stress are different from that of the Earth's rotation. We prove a convergence result for a three-dimensional NavierStokesCoriolis system in a bounded domain, in the asymptotic of fast rotation and vanishing vertical viscosity, and we exhibit some random and stationary boundary layer profiles. At last, an average equation is derived for the limit system in the case of the nonresonant torus. |
| Starting Page | 511 |
| Ending Page | 563 |
| Page Count | 53 |
| File Format | |
| ISSN | 00361410 |
| DOI | 10.1137/080718139 |
| e-ISSN | 10957154 |
| Journal | SIAM Journal on Mathematical Analysis (SJMAAH) |
| Issue Number | 2 |
| Volume Number | 41 |
| Language | English |
| Publisher | Society for Industrial and Applied Mathematics |
| Publisher Date | 2009-05-14 |
| Access Restriction | Subscribed |
| Subject Keyword | Rotating fluids Hydrology, hydrography, oceanography boundary layer oceanic circulation rotating fluids stationary setting Partial differential equations with randomness, stochastic partial differential equations Asymptotic behavior of solutions |
| Content Type | Text |
| Resource Type | Article |
| Subject | Applied Mathematics Analysis Computational Mathematics |
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