Linear inviscid damping for stably stratified Boussinesq flows

TL;DR

This paper analyzes the linear stability of stratified shear flows in the Boussinesq system, revealing decay rates and spectral properties that depend on stratification regimes and critical thresholds.

Contribution

It provides a detailed description of inviscid damping and spectral analysis for stratified Boussinesq flows, including stratification-dependent decay rates and the continuous spectrum result.

Findings

Velocity and density decay estimates depend on stratification regimes.

Vorticity and density gradient grow sub-linearly over time.

Spectrum of the linearized operator is purely continuous under mild conditions.

Abstract

We study the linear asymptotic stability of stably stratified monotone shear flows for the Boussinesq equations in the periodic channel. By means of the limiting absorption principle, we obtain a precise description of the inviscid damping experienced by the perturbed velocity field and density, with time-decay rates that depend on the local Richardson number $\mathcal{J}(y)$ and split into four stratification regimes (non-stratified, weak, mild, and strong) reflecting qualitative changes in the structure of the Green's function at the critical thresholds $\mathcal{J}(y)=0$ and $\mathcal{J}(y) = \frac14$. The velocity and density decay estimates are later used to prove quantitative sub-linear growth of the vorticity and gradient of density. As a byproduct of our analysis, we show that, under mild hypotheses on the underlying shear-type equilibrium, the spectrum of the linearised Boussinesq operator is purely continuous.