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.
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