Non-uniqueness of forced active scalar equations with even drift operators
From MaRDI portal
Publication:6584201
DOI10.1016/j.physd.2024.134271zbMath1542.35309MaRDI QIDQ6584201
Susan J. Friedlander, Mimi Dai
Publication date: 6 August 2024
Published in: Physica D (Search for Journal in Brave)
PDEs in connection with fluid mechanics (35Q35) Existence, uniqueness, and regularity theory for incompressible viscous fluids (76D03) PDEs in connection with geophysics (35Q86)
Cites Work
- Unnamed Item
- Dissipative continuous Euler flows
- Dissipative Euler flows and Onsager's conjecture
- Global well-posedness for an advection-diffusion equation arising in magneto-geostrophic dynamics
- Lack of uniqueness for weak solutions of the incompressible porous media equation
- Global well-posedness for the critical 2D dissipative quasi-geostrophic equation
- The Euler equations as a differential inclusion
- Drift diffusion equations with fractional diffusion and the quasi-geostrophic equation
- A proof of Onsager's conjecture
- Hölder continuous solutions of active scalar equations
- Nonuniqueness of weak solutions to the Navier-Stokes equation
- Nonlinear maximum principles for dissipative linear nonlocal operators and applications
- Non-uniqueness of steady-state weak solutions to the surface quasi-geostrophic equations
- Localized mixing zone for Muskat bubbles and turned interfaces
- Mixing solutions for the Muskat problem
- Anomalous dissipation for \(1/5\)-Hölder Euler flows
- Existence and regularity of weak solutions to the quasi-geostrophic equations in the spaces \(L^p\) or \(\dot{H}^{-1/2}\)
- Dissipative Euler Flows with Onsager-Critical Spatial Regularity
- On the ill/well-posedness and nonlinear instability of the magneto-geostrophic equations
- Convex integration for a class of active scalar equations
- Analytical behavior of two-dimensional incompressible flow in porous media
- Formation of strong fronts in the 2-D quasigeostrophic thermal active scalar
- Relaxation of the incompressible porous media equation
- On the supercritically diffusive magnetogeostrophic equations
- A direct approach to nonuniqueness and failure of compactness for the SQG equation
- Nonuniqueness of Weak Solutions to the SQG Equation
- Magnetostrophic Turbulence and the Geodynamo
- Nonuniqueness of Leray–Hopf solutions for a dyadic model
Related Items (1)
This page was built for publication: Non-uniqueness of forced active scalar equations with even drift operators