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dc.contributor.authorDritschel, D.G.
dc.contributor.authorLucia, M.
dc.contributor.authorPoje, A.C.
dc.date.accessioned2015-07-24T11:10:01Z
dc.date.available2015-07-24T11:10:01Z
dc.date.issued2015-06-29
dc.identifier.citationDritschel , D G , Lucia , M & Poje , A C 2015 , ' Ergodicity and spectral cascades in point vortex flows on the sphere ' , Physical Review. E, Statistical, nonlinear, and soft matter physics , vol. 91 , no. 6 , 063014 . https://doi.org/10.1103/PhysRevE.91.063014en
dc.identifier.issn1539-3755
dc.identifier.otherPURE: 204815954
dc.identifier.otherPURE UUID: 4fa8ed7e-c84b-4126-a12b-a6c2a2497269
dc.identifier.otherScopus: 84936971656
dc.identifier.otherWOS: 000357028500015
dc.identifier.otherORCID: /0000-0001-6489-3395/work/64697792
dc.identifier.urihttps://hdl.handle.net/10023/7024
dc.descriptionA.C.P. was supported under DOD (MURI) Grant No. N000141110087 ONR. The computations were supported by the CUNY HPCC under NSF Grants No. CNS-0855217 and No. CNS-0958379.en
dc.description.abstractWe present results for the equilibrium statistics and dynamic evolution of moderately large [n = O (102 - 103)] numbers of interacting point vortices on the sphere under the constraint of zero mean angular momentum. For systems with equal numbers of positive and negative identical circulations, the density of rescaled energies, p(E), converges rapidly with n to a function with a single maximum with maximum entropy. Ensemble-averaged wave-number spectra of the nonsingular velocity field induced by the vortices exhibit the expected k-1 behavior at small scales for all energies. Spectra at the largest scales vary continuously with the inverse temperature of the system. For positive temperatures, spectra peak at finite intermediate wave numbers; for negative temperatures, spectra decrease everywhere. Comparisons of time and ensemble averages, over a large range of energies, strongly support ergodicity in the dynamics even for highly atypical initial vortex configurations. Crucially, rapid relaxation of spectra toward the microcanonical average implies that the direction of any spectral cascade process depends only on the relative difference between the initial spectrum and the ensemble mean spectrum at that energy, not on the energy, or temperature, of the system.
dc.format.extent7
dc.language.isoeng
dc.relation.ispartofPhysical Review. E, Statistical, nonlinear, and soft matter physicsen
dc.rights© 2015 American Physical Society. Reproduced in accordance with the Publisher's author reuse policy. Originally published by Physical Review E: http://dx.doi.org/10.1103/PhysRevE.91.063014en
dc.subjectQC Physicsen
dc.subjectNDASen
dc.subjectBDCen
dc.subject.lccQCen
dc.titleErgodicity and spectral cascades in point vortex flows on the sphereen
dc.typeJournal articleen
dc.description.versionPublisher PDFen
dc.contributor.institutionUniversity of St Andrews. Applied Mathematicsen
dc.contributor.institutionUniversity of St Andrews. Marine Alliance for Science & Technology Scotlanden
dc.contributor.institutionUniversity of St Andrews. Scottish Oceans Instituteen
dc.identifier.doihttps://doi.org/10.1103/PhysRevE.91.063014
dc.description.statusPeer revieweden


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