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Time quasi-periodic vortex patches for quasi-geostrophic shallow-water equations
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In this paper, we shall implement KAM theory in order to construct a large class of time quasi-periodic solutions for an active scalar model arising in fluid dynamics. More precisely, the construction of invariant tori is performed for quasi-geostrophic shallow-water equations when the {\it Rossby deformation length} belongs to a massive Cantor set. As a consequence, we construct pulsating vortex patches whose boundary is localized in a thin annulus for any time.
Forward citations
Cited by 4 Pith papers
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Time Quasi-Periodic Three-dimensional Traveling Gravity Water Waves
Existence of small-amplitude, linearly stable, time quasi-periodic traveling solutions for 3D pure gravity water waves in finite depth on tori, for generic lattices and most depths.
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Time-periodic vortices near translating symmetric dipole patches
Non-rigid time-periodic vortex patch solutions bifurcating from translating symmetric dipoles are constructed for the 2D Euler equations using Lyapunov-Schmidt reduction and Nash-Moser methods.
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On stationary Quasi-Geostrophic Shallow-Water flows
Non-trivial m-fold doubly-connected stationary vortex patches are proven to exist for the quasi-geostrophic shallow-water equations via bifurcation from annuli.
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The regularity of the boundary of vortex patches for the quasi-geostrophic shallow-water equations
For the QGSW equations, a C^{1,γ} vortex patch boundary stays C^{1,γ} for all time, and as the inverse Rossby radius ε→0 the solutions converge to 2D Euler in little Hölder spaces on a uniform time interval.
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