2002
DOI: 10.1063/1.1459755
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Enstrophy dynamics of stochastically forced large-scale geophysical flows

Abstract: Enstrophy is an averaged measure of fluid vorticity. This quantity is particularly important in rotating geophysical flows. We investigate the dynamical evolution of enstrophy for large-scale quasi-geostrophic flows under random wind forcing. We obtain upper bounds on the enstrophy, as well as results establishing its Hölder continuity and describing the small-time asymptotics.

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Cited by 4 publications
(3 citation statements)
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References 26 publications
(50 reference statements)
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“…Furthermore, we show that for t → 0 the linear regime dominates. In [3] also H"older-continuity for the mean energy was shown for a quasigeostrophic model. We conclude this section by a qualitative discussion on upper bounds for the energy using additive and multiplicative trace-class noise.…”
Section: Nonlinear Theorymentioning
confidence: 94%
See 1 more Smart Citation
“…Furthermore, we show that for t → 0 the linear regime dominates. In [3] also H"older-continuity for the mean energy was shown for a quasigeostrophic model. We conclude this section by a qualitative discussion on upper bounds for the energy using additive and multiplicative trace-class noise.…”
Section: Nonlinear Theorymentioning
confidence: 94%
“…Here we rely on a much simpler tool, which can also be applied to other equations. See for instance [3] for a quasigeostrophic model, where our analysis would apply, too.…”
Section: Body Forcing -Mean Energy Boundsmentioning
confidence: 99%
“…For other ocean models, the reader is referred to [4,5,[10][11][12][13][14] for the mathematical study, and to [15,16,21,22] for the physical background, among others.…”
Section: Introductionmentioning
confidence: 99%