The limit of small Rossby numbers for randomly forced quasi-geostrophic equation on $\beta$-plane
Sergei Kuksin, Alberto Maiocchi

TL;DR
This paper analyzes the behavior of the 2D quasigeostrophic equation on the $eta$-plane with random forcing, showing that as $eta$ becomes large, the solution's action-vector law converges to that of an effective integrable system, with no energy cascade observed.
Contribution
It establishes the convergence of the solution's action-vector law to an effective integrable system as $eta o \infty$, including uniformity in dissipation parameter $\kappa$.
Findings
Action-vector law converges to an effective system as $eta o \infty$
Stationary distribution converges to that of the effective system
No energy cascade to high frequencies in the limiting systems
Abstract
We consider the 2d quasigeostrophic equation on the -plane for the stream function , with dissipation and a random force: where . For typical values of the horizontal period we prove that the law of the action-vector of a solution for (formed by the halves of the squared norms of its complex Fourier coefficients) converges, as , to the law of an action-vector for solution of an auxiliary effective equation, and the stationary distribution of the action-vector for solutions of converges to that of the effective equation. Moreover, this convergence is uniform in . The effective equation is an infinite…
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Taxonomy
TopicsNavier-Stokes equation solutions · Stochastic processes and statistical mechanics
