Statistical mechanics of two-dimensional and geophysical flows

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• 作者：Freddy Bouchet^a ; ^{Freddy.Bouchet@ens-lyon.fr} ; Antoine Venaille^b
• 关键词：2D Euler equations ; Large scales of turbulent flows ; 2D turbulence ; Quasi-geostrophic equations ; Geophysical turbulence ; Statistical mechanics ; Long range interactions ; Kinetic theory ; Jupiter&rsquo ; s troposphere ; Great Red Spot ; Ocean jets ; Ocean rings
• 刊名：Physics Reports
• 出版年：2012
• 期刊代码：59_03701573
• 类别：ph
• 出版时间：June, 2012
• 卷：515
• 期：5
• 页码：227-295
• 文件大小：4836 K

摘要

The theoretical study of the self-organization of two-dimensional and geophysical turbulent flows is addressed based on statistical mechanics methods. This review is a self-contained presentation of classical and recent works on this subject; from the statistical mechanics basis of the theory up to applications to Jupiter鈥檚 troposphere and ocean vortices and jets. Emphasize has been placed on examples with available analytical treatment in order to favor better understanding of the physics and dynamics.

After a brief presentation of the 2D Euler and quasi-geostrophic equations, the specificity of two-dimensional and geophysical turbulence is emphasized. The equilibrium microcanonical measure is built from the Liouville theorem. Important statistical mechanics concepts (large deviations and mean field approach) and thermodynamic concepts (ensemble inequivalence and negative heat capacity) are briefly explained and described.

On this theoretical basis, we predict the output of the long time evolution of complex turbulent flows as statistical equilibria. This is applied to make quantitative models of two-dimensional turbulence, the Great Red Spot and other Jovian vortices, ocean jets like the Gulf-Stream, and ocean vortices. A detailed comparison between these statistical equilibria and real flow observations is provided.

We also present recent results for non-equilibrium situations, for the studies of either the relaxation towards equilibrium or non-equilibrium steady states. In this last case, forces and dissipation are in a statistical balance; fluxes of conserved quantity characterize the system and microcanonical or other equilibrium measures no longer describe the system.