Global weak solutions to the inviscid 3D quasi-geostrophic equation
From MaRDI portal
Publication:496201
DOI10.1007/s00220-015-2428-3zbMath1328.35177arXiv1412.4522OpenAlexW3098052860MaRDI QIDQ496201
Marjolaine Puel, Alexis F. Vasseur
Publication date: 21 September 2015
Published in: Communications in Mathematical Physics (Search for Journal in Brave)
Full work available at URL: https://arxiv.org/abs/1412.4522
PDEs in connection with fluid mechanics (35Q35) Hydrology, hydrography, oceanography (86A05) Weak solutions to PDEs (35D30) PDEs in connection with geophysics (35Q86)
Related Items
On the well-posedness of the inviscid multi-layer quasi-geostrophic equations ⋮ Global in time classical solutions to the 3D quasi-geostrophic system for large initial data ⋮ Nonuniqueness of Weak Solutions to the 3 Dimensional Quasi-Geostrophic Equations ⋮ The inviscid three dimensional quasi-geostrophic system on bounded domains ⋮ The Barotropic Quasi-Geostrophic Equation under a Free Surface ⋮ On the Weak Solutions to the Three-Dimensional Inviscid Quasi-Geostrophic System ⋮ Classical solutions for the 3D quasi-geostrophic system on a bounded domain
Cites Work
- Unnamed Item
- Unnamed Item
- Derivation of quasi-geostrophic potential vorticity equations
- Testing the limits of quasi-geostrophic theory: application to observed laboratory flows outside the quasi-geostrophic regime
- Euler Equations, Navier-Stokes Equations and Turbulence
- Validity of the Quasigeostrophic Model for Large-Scale Flow in the Atmosphere and Ocean
- Formation of strong fronts in the 2-D quasigeostrophic thermal active scalar
- Surface quasi-geostrophic dynamics