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We establish the nonlinear stability on a timescale O (^-2) of a linearly, stably stratified rest state in the inviscid Boussinesq system on R². Here >0 denotes the size of an initially sufficiently small, Sobolev regular and localized perturbation. A similar statement also holds for the related dispersive SQG equation. At the core of this result is a dispersive effect due to anisotropic internal gravity waves. At the linearized level, this gives rise to amplitude decay at a rate of t^-1/2, as observed in EW15. We establish a refined version of this, and propagate nonlinear control via a detailed analysis of nonlinear interactions using the method of partial symmetries developed in GPW23.
Jurja et al. (Tue,) studied this question.
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