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Role of weak Casimirs in constraining stratified thermal IL^{(0,1)}QG flow

Determine the role of the weak Casimir integrals of motion I_F[bar{ξ},ψ_σ,ψ_{σ^2}] = ∫_𝒟 bar{ξ} F(ψ_σ − (2/3) ψ_{σ^2}) d^2x in constraining the dynamics of the stratified thermal quasigeostrophic model IL^{(0,1)}QG, including whether and how these integrals can be used to derive formal or Lyapunov stability conditions or other invariant bounds for stratified flows.

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Background

In the IL{(0,1)}QG model, the authors identify an infinite family of conserved quantities I_F = ∫ bar{ξ} F(ψσ − (2/3) ψ2}) d2x, which they term weak Casimirs because they do not lie in the kernel of the full Lie–Poisson bracket for (bar{ξ}, ψσ, ψ2}), although they do form the kernel for a reduced bracket involving (bar{ξ}, χ) with χ := ψσ − (2/3) ψ2}.

While standard energy–Casimir methods (Arnold’s method) successfully yield formal and Lyapunov stability for certain basic states, attempts to include the weak Casimirs did not produce positive-definite pseudoenergy–momentum functionals except in a restrictive case. The authors therefore highlight that the dynamical significance of these weak Casimirs for constraining stratified flows in IL{(0,1)}QG remains unresolved.

References

Only a subset of such states was found Lyapunov stable using the available integrals, except the weak Casimirs, whose role in constraining stratified thermal flow remains to be understood.

Properties and baroclinic instability of stratified thermal upper-ocean flow (2403.18084 - Beron-Vera et al., 26 Mar 2024) in Abstract