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arXiv · 2611.00964

Stability threshold for 3D Boussinesq equations with rotation near the Couette flow and vertical stratified temperature

Abstract

The most important features that distinguish fluid flow in the atmosphere and ocean are the effects of rotation and stratification, which are described by the Boussinesq equations with rotation. This paper examines the stability threshold at high Reynolds number $\mathbf{Re}$ for the 3D Boussinesq equations with rotation near Couette flow and a vertical stratified temperature. For the zero modes, the combined effects of rotation and stratification sustain velocity-temperature oscillations with frequencies bounded away from zero. In the stable rotational regime, rotation suppresses the linear growth associated with the lift-up effect, while stratification sustains oscillations in the double zero modes. Although the zero modes dynamics are not fully dispersive, we exploit the structure of the oscillatory phases and cancellations in the equations to obtain a modified energy estimate for the entire zero modes system. Combining this estimate with enhanced dissipation and inviscid damping of the nonzero modes, we establish a bound for the stability threshold, with order $\mathbf{Re}^{-2/3}(1+\log\mathbf{Re})^{-1-a_0}$ for any fixed $a_0\in(0,1/2)$.

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Wenting Huang, Zekai Luo, Ying Sun, Jiahong Wu, Xiaojing Xu. 2026-10-31. Stability threshold for 3D Boussinesq equations with rotation near the Couette flow and vertical stratified temperature. https://arxiv.org/abs/2611.00964

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