Quasi-geostrophy against the wall

Coasts are obstructions to the classical derivation of continuously stratified quasigeostrophic equations, due to possible resonances between slow internal coastally trapped Kelvin waves and anticyclones. [Deremble et al Ocean Modelling 2017] proposed a coupled model between a quasigeostrophic interior and boundary layer Kelvin wave dynamics. We revisit the derivation of this model, paying particular attention to conservation laws. We find that quasigeostrophic energy is conserved despite the existence of Kelvin wave shocks in the boundary layer. The effect of those shocks is to change the global distribution of potential vorticity, and, consequently the interior flow structure. In that respect, we show that there is an active control of the boundary region on the interior flow.