Global Existence, Hamiltonian Conservation and Vanishing Viscosity for the Surface Quasi-Geostrophic Equation

Fuente: arXiv
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Main Authors: De Rosa, Luigi, Latocca, Mickaël, Park, Jaemin
Format: Preprint
Published: 2025
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_version_ 1866912563614187520
author De Rosa, Luigi
Latocca, Mickaël
Park, Jaemin
author_facet De Rosa, Luigi
Latocca, Mickaël
Park, Jaemin
contents For any initial datum $θ_0\in L^{\frac{4}{3}}_x$ it is proved the existence of a global-in-time weak solution $θ\in L^\infty_t L^{\frac43}_x$ to the surface quasi-geostrophic equation whose Hamiltonian, i.e. the $\dot{H}^{-\frac{1}{2}}_x$ 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 $L^{\frac{4}{3}}_x$ 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.
format Preprint
id arxiv_https___arxiv_org_abs_2509_01268
institution arXiv
publishDate 2025
record_format arxiv
spellingShingle Global Existence, Hamiltonian Conservation and Vanishing Viscosity for the Surface Quasi-Geostrophic Equation
De Rosa, Luigi
Latocca, Mickaël
Park, Jaemin
Analysis of PDEs
For any initial datum $θ_0\in L^{\frac{4}{3}}_x$ it is proved the existence of a global-in-time weak solution $θ\in L^\infty_t L^{\frac43}_x$ to the surface quasi-geostrophic equation whose Hamiltonian, i.e. the $\dot{H}^{-\frac{1}{2}}_x$ 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 $L^{\frac{4}{3}}_x$ 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.
title Global Existence, Hamiltonian Conservation and Vanishing Viscosity for the Surface Quasi-Geostrophic Equation
topic Analysis of PDEs
url https://arxiv.org/abs/2509.01268