Large-scale dissipation and filament instability in two-dimensional turbulence (Articolo in rivista)

Type
Label
  • Large-scale dissipation and filament instability in two-dimensional turbulence (Articolo in rivista) (literal)
Anno
  • 2005-01-01T00:00:00+01:00 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
  • 10.1103/PhysRevLett.95.014503 (literal)
Alternative label
  • D. Elhmaidi, J. von Hardenberg, A. Provenzale (2005)
    Large-scale dissipation and filament instability in two-dimensional turbulence
    in Physical review letters (Print)
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • D. Elhmaidi, J. von Hardenberg, A. Provenzale (literal)
Pagina inizio
  • 14503 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
  • 95 (literal)
Rivista
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroFascicolo
  • 1 (literal)
Note
  • ISI Web of Science (WOS) (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • Fac Sci Tunis, Lab Mecan Fluides, Tunis 1060, Tunisia (Elhmaidi) ISAC-CNR, Torino, Italy (Provenzale, von Hardenberg) (literal)
Titolo
  • Large-scale dissipation and filament instability in two-dimensional turbulence (literal)
Abstract
  • Coherent vortices in two-dimensional turbulence induce far-field effects that stabilize vorticity filaments and inhibit the generation of new vortices. We show that the large-scale energy sink often included in numerical simulations of statistically stationary two-dimensional turbulence reduces the stabilizing role of the vortices, leading to filament instability and to continuous formation of new coherent vortices. This counter-intuitive effect sheds new light on the mechanisms responsible for vortex formation in forced-dissipated two-dimensional turbulence and it has significant impact on the temporal evolution of the vortex population in freely-decaying turbulence. The time dependence of vortex statistics in the presence of a large-scale energy sink can be approximately described by a modified version of the scaling theory developed for small-scale dissipation. (literal)
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