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Nonexistence of simple hyperbolic blow-up for the quasi-geostrophic equation

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TLDR
In this article, it was shown that the saddle cannot close in finite time and it cannot be faster than a double exponential in time, and the same results hold for incompressible 2D and 3D Euler vorticity equations.
Abstract
The problem we are concerned with is whether singularities form in finite time in incompressible fluid flows. It is well known that the answer is ``no'' in the case of Euler and Navier-Stokes equations in dimension two. In dimension three it is still an open problem for these equations. In this paper we focus on a two-dimensional active scalar model for the 3D Euler vorticity equation. Constantin, Majda and Tabak suggested, by studying rigorous theorems and detailed numerical experiments, a general principle: ``If the level set topology in the temperature field for the 2D quasi-geostrophic active scalar in the region of strong scalar gradients does not contain a hyperbolic saddle, then no finite time singularity is possible.'' Numerical simulations showed evidence of singular behavior when the geometry of the level sets of the active scalar contain a hyperbolic saddle. There is a naturally associated notion of simple hyperbolic saddle breakdown. The main theorem we present in this paper shows that such breakdown cannot occur in finite time. We also show that the angle of the saddle cannot close in finite time and it cannot be faster than a double exponential in time. Using the same techniques, we see that analogous results hold for incompressible 2D and 3D Euler.

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Citations
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Hitchhiker's guide to the fractional Sobolev spaces

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Geophysical fluid dynamics.

James R. Holton
- 28 Jan 1983 - 
TL;DR: Specialized experiments with atmosphere and coupled models show that the main damping mechanism for sea ice region surface temperature is reduced upward heat flux through the adjacent ice-free oceans resulting in reduced atmospheric heat transport into the region.
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A Maximum Principle Applied to Quasi-Geostrophic Equations

TL;DR: In this paper, the authors study the initial value problem for dissipative 2D quasi-geostrophic equations proving local existence, global results for small initial data in the super-critical case, decay of Lp-norms and asymptotic behavior of viscosity solution in the critical case.
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On the Euler equations of incompressible fluids

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From the long jump random walk to the fractional Laplacian

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References
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Book

Geophysical Fluid Dynamics

TL;DR: In this article, the authors propose a quasigeostrophic motion of a Stratified Fluid on a Sphere (SFL) on a sphere, which is based on an Inviscid Shallow-Water Theory.
Journal ArticleDOI

Remarks on the breakdown of smooth solutions for the 3- D Euler equations

TL;DR: In this article, the authors prove that the maximum norm of the vorticity of a solution of the Euler equation is a function of the smoothness of the solution, and that if a solution is initially smooth and loses its regularity at some later time, then the maximum vortivity necessarily grows without bound as the critical time approaches.
Journal ArticleDOI

Geophysical fluid dynamics.

James R. Holton
- 28 Jan 1983 - 
TL;DR: Specialized experiments with atmosphere and coupled models show that the main damping mechanism for sea ice region surface temperature is reduced upward heat flux through the adjacent ice-free oceans resulting in reduced atmospheric heat transport into the region.
Journal ArticleDOI

Formation of strong fronts in the 2-D quasigeostrophic thermal active scalar

TL;DR: In this paper, the formation of strong and potentially singular fronts in a two-dimensional quasigeostrophic active scalar is studied through the symbiotic interaction of mathematical theory and numerical experiments.
Journal ArticleDOI

Geometric statistics in turbulence

Peter Constantin
- 01 Mar 1994 - 
TL;DR: The author presents results concerning scaling exponents in turbulence and estimates the average dissipation rate, the average dimension of level sets, and a class of two-dimensional equations that are useful models of incompressible dynamics.
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