Stability and exponential decay for the 2D anisotropic Boussinesq equations with horizontal dissipation

TL;DR

This paper proves the stability and exponential decay of perturbations in a 2D anisotropic Boussinesq system with only horizontal dissipation, clarifying large-time behavior near hydrostatic equilibrium on certain domains.

Contribution

It establishes the global stability and decay rates for the anisotropic Boussinesq equations with horizontal dissipation on the domain rac{ ext{T}}{ ext{R}}, solving an open problem in Sobolev spaces.

Findings

Oscillations decay exponentially in H^1

Solutions converge to horizontal averages

Stability proven in Sobolev space H^2

Abstract

The hydrostatic equilibrium is a prominent topic in fluid dynamics and astrophysics. Understanding the stability of perturbations near the hydrostatic equilibrium of the Boussinesq systems helps gain insight into certain weather phenomena. The 2D Boussinesq system focused here is anisotropic and involves only horizontal dissipation and horizontal thermal diffusion. Due to the lack of the vertical dissipation, the stability and precise large-time behavior problem is difficult. When the spatial domain is $\mathbb R^2$, the stability problem in a Sobolev setting remains open. When the spatial domain is $\mathbb T\times \mathbb R$, this paper solves the stability problem and specifies the precise large-time behavior of the perturbation. By decomposing the velocity $u$ and temperature $\theta$ into the horizontal average $(\bar u, \bar\theta)$ and the corresponding oscillation $(\widetilde u, \widetilde \theta)$, and deriving various anisotropic inequalities, we are able to establish the global stability in the Sobolev space $H^2$. In addition, we prove that the oscillation $(\widetilde u, \widetilde \theta)$ decays exponentially to zero in $H^1$ and $(u, \theta)$ converges to $(\bar u, \bar\theta)$. This result reflects the stratification phenomenon of buoyancy-driven fluids.