On the forced surface quasi-geostrophic equation: Existence of steady states and sharp relaxation rates

TL;DR

This paper studies the forced surface quasi-geostrophic equation, proving existence of steady states, their attraction properties, and sharp relaxation rates for solutions with localized initial data.

Contribution

It constructs steady states under minimal forcing assumptions and establishes convergence and sharp relaxation rates for solutions of the forced SQG equation.

Findings

Existence of steady states for the forced SQG equation.

Global solutions converge to steady states in L^p spaces.

Sharp relaxation rates are computed for localized initial data.

Abstract

We consider the asymptotic behavior of the surface quasi-geostrophic equation, subject to a small external force. Under suitable assumptions on the forcing, we first construct the steady states and we provide a number of useful a posteriori estimates for them. Importantly, to do so, we only impose minimal cancellation conditions on the forcing function. Our main result is that all $L^1\cap L^\infty$ localized initial data produces global solutions of the forced SQG, which converge to the steady states in $L^p(\mathbf R^2), 1<p\leq 2$ as time goes to infinity. This establishes that the steady states serve as one point attracting set. Moreover, by employing the method of scaling variables, we compute the sharp relaxation rates, by requiring slightly more localized initial data.