Impeded inverse energy transfer in the Charney Hasegawa Mima model of quasi-geostrophic flows

The behaviour of turbulent flows within the single-layer quasi-geostrophic (Charney Hasegawa Mima) model is shown to be strongly dependent on the Rossby deformation wavenumber lambda (or free-surface elasticity). Herein, we derive a bound on the inverse energy transfer, specifically on the growth rate dℓ/d t of the characteristic length scale ℓ representing the energy centroid. It is found that dℓ/d t≤2\|q\|_infty/(ℓ_slambda(2)) , where \|q\|_infty is the supremum of the potential vorticity and ℓ_s represents the potential enstrophy centroid of the reservoir, both invariant. This result implies that in the potential-energy-dominated regime (ℓ≥ℓ_s {≫} lambda(-1) ), the inverse energy transfer is strongly impeded, in the sense that under the usual time scale no significant transfer of energy to larger scales occurs. The physical implication is that the elasticity of the free surface impedes turbulent energy transfer in wavenumber space, effectively rendering large-scale vortices long-lived and inactive. Results from numerical simulations of forced-dissipative turbulence confirm this prediction.