2025/09/01 by De Rosa, Luigi, Latocca, Mickaël, Park, Jaemin · 1 citation
#Analysis of PDEs (math.AP) #FOS: Mathematics
paper · doi:10.48550/arxiv.2509.01268
For any initial datum θ0∈ L(4)/(3)x it is proved the existence of a global-in-time weak solution θ∈ L^∞t L\frac43x to the surface quasi-geostrophic equation whose Hamiltonian, i.e. the H-(1)/(2)x norm, is constant in time. The solution is obtained as a vanishing viscosity limit. Outside the classical strong compactness setting, the main idea is to propagate in time the non-concentration of the L(4)/(3)x norm of the initial data, from which strong compactness in the Hamiltonian norm is deduced. General no anomalous dissipation results under minimal Onsager supercritical assumptions are also obtained.