A logarithmically improved regularity criterion for the surface quasi-geostrophic equation
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Publication:1732405
DOI10.1016/j.camwa.2017.11.004zbMath1409.76026OpenAlexW2770521204MaRDI QIDQ1732405
Publication date: 25 March 2019
Published in: Computers \& Mathematics with Applications (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1016/j.camwa.2017.11.004
Navier-Stokes equations for incompressible viscous fluids (76D05) Hydrology, hydrography, oceanography (86A05) PDEs in connection with geophysics (35Q86)
Cites Work
- Unnamed Item
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- A regularity criterion for the dissipative quasi-geostrophic equations
- A discrete transform and decompositions of distribution spaces
- Global well-posedness for the critical 2D dissipative quasi-geostrophic equation
- Regularity of Hölder continuous solutions of the supercritical quasi-geostrophic equation
- Drift diffusion equations with fractional diffusion and the quasi-geostrophic equation
- A regularity criterion for the critical and supercritical dissipative quasi-geostrophic equations
- Regularity condition of solutions to the quasi-geostrophic equations in Besov spaces with negative indices
- A remark on regularity criterion for the dissipative quasi-geostrophic equations
- Hölder continuity of solutions of supercritical dissipative hydrodynamic transport equations
- Regularity criteria for the dissipative quasi-geostrophic equations in Hölder spaces
- The critical Sobolev inequalities in Besov spaces and regularity criterion to some semi-linear evolution equations
- Bilinear estimates in \(BMO\) and the Navier-Stokes equations
- Nonlinear maximum principles for dissipative linear nonlocal operators and applications
- Variation on a theme of Caffarelli and Vasseur
- Remarks on the global regularity for the super-critical 2D dissipative quasi-geostrophic equation
- On regularity criterion for the dissipative quasi-geostrophic equations
- The maximum principle and the global attractor for the dissipative 2D quasi-geostrophic equations
- Fourier Analysis and Nonlinear Partial Differential Equations
- Well‐posedness and scattering results for the generalized korteweg‐de vries equation via the contraction principle
- Formation of strong fronts in the 2-D quasigeostrophic thermal active scalar
- Behavior of Solutions of 2D Quasi-Geostrophic Equations
- On the Regularity Conditions for the Dissipative Quasi-geostrophic Equations
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