Year: 2011
Journal of Partial Differential Equations, Vol. 24 (2011), Iss. 1 : pp. 15–36
Abstract
In this paper, the two-layer quasigeostrophic flow model under stochastic wind forcing is considered. It is shown that when the layer depth or density difference across the layers tends to zero, the dynamics on both layers synchronizes to an averaged geophysical flow model.
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Journal Article Details
Publisher Name: Global Science Press
Language: English
DOI: https://doi.org/10.4208/jpde.v24.n1.2
Journal of Partial Differential Equations, Vol. 24 (2011), Iss. 1 : pp. 15–36
Published online: 2011-01
AMS Subject Headings:
Copyright: COPYRIGHT: © Global Science Press
Pages: 22
Keywords: Stochastic flow models