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Properties and baroclinic instability of stratified thermal upper-ocean flow

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arXiv:2403.18084v1 Announce Type: cross
Abstract: We study the properties of, and perform a stability analysis of a baroclinic zonal current in, a thermal rotating shallow-water model, sometimes called \emph{Ripa's model}, featuring stratification for quasigeostrophic upper-ocean dynamics. The model has Lie--Poisson Hamiltonian structure. In addition to Casimirs, the model supports integrals of motion that neither form the kernel of the bracket nor are related to explicit symmetries. The model sustains Rossby waves and a neutral model, whose spurious growth is prevented by a positive-definite integral, quadratic on the deviation from the motionless state. A baroclinic zonal jet with vertical curvature is found to be spectrally stable for specific configurations of the gradients of layer thickness, vertically averaged buoyancy, and buoyancy frequency. Only a subset of such states was found Lyapunov stable using the available integrals, except the newly reported ones, whose role in constraining stratified thermal flow remains elusive. The existence of Lyapunov-stable states enabled bounding the nonlinear growth of perturbations to spectrally unstable states. Our results do not support the generality of earlier numerical evidence on the suppression of submesoscale wave activity as a result of the inclusion of stratification in thermal shallow-water theory, which we supported with direct numerical simulations.

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