2013
DOI: 10.1007/s10955-013-0809-6
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Additional Invariants and Statistical Equilibria for the 2D Euler Equations on a Spherical Domain

Abstract: The role of the domain geometry for the statistical mechanics of 2D Euler flows is investigated. It is shown that for a spherical domain, there exists invariant subspaces in phase space which yield additional angular momentum, energy and enstrophy invariants. The microcanonical measure taking into account these invariants is built and a mean-field, Robert-Sommeria-Miller theory is developed in the simple case of the energy-enstrophy measure. The variational problem is solved analytically and a partial energy c… Show more

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Cited by 15 publications
(42 citation statements)
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“…Different geometries can be studied: in a rotating sphere, the equilibria, in the linear limit, can be either solid‐body rotations, dipole flows [ Herbert et al , ], or quadrupoles, taking into account conservation of angular momentum [ Herbert , ]. In the latter case, a perturbative treatment of the nonlinearity in the falseω¯falseψ¯ relationship leads to the same flow topology, but sharper vortex cores [ Qi and Marston , ].…”
Section: Equilibrium Statistical Mechanics For Geophysical Flowsmentioning
confidence: 99%
“…Different geometries can be studied: in a rotating sphere, the equilibria, in the linear limit, can be either solid‐body rotations, dipole flows [ Herbert et al , ], or quadrupoles, taking into account conservation of angular momentum [ Herbert , ]. In the latter case, a perturbative treatment of the nonlinearity in the falseω¯falseψ¯ relationship leads to the same flow topology, but sharper vortex cores [ Qi and Marston , ].…”
Section: Equilibrium Statistical Mechanics For Geophysical Flowsmentioning
confidence: 99%
“…Equilibrium statistical mechanics of twodimensional and quasi-geostrophic flows is now fairly well understood. It has been applied to various problems in geophysical context such as the description of Jovian vortices [44,3], oceanic rings and jets [50,55], equilibria on a sphere [15], and to describe the vertical energy partition in continuously stratified quasi-geostrophic flows [19,52,48].…”
Section: Introductionmentioning
confidence: 99%
“…nm , (39) given that neither denominators vanish. Finally, the critical points in this case are superpositions of a solid-body rotation and a multipole in each layer:…”
Section: Degenerate Casesmentioning
confidence: 99%