Frictional dissipation at the interface of a two-layer quasi-geostrophic flow (Articolo in rivista)

Type
Label
  • Frictional dissipation at the interface of a two-layer quasi-geostrophic flow (Articolo in rivista) (literal)
Anno
  • 2008-01-01T00:00:00+01:00 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
  • 10.1393/ncc/i2008-10299-y (literal)
Alternative label
  • Crisciani F. (1), Purini R. (2), Severini M. (3) (2008)
    Frictional dissipation at the interface of a two-layer quasi-geostrophic flow
    in Il Nuovo cimento della Società italiana di fisica. C. Geophysics and space physics (Testo stamp.)
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • Crisciani F. (1), Purini R. (2), Severini M. (3) (literal)
Pagina inizio
  • 327 (literal)
Pagina fine
  • 337 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
  • 31 (literal)
Rivista
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroFascicolo
  • 3 (literal)
Note
  • Scopu (literal)
  • ISI Web of Science (WOS) (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • (1) CNR, ISMAR, I-34123 Trieste, Italy (2) CNR, ISAC, I-00133 Rome, Italy (3) Univ Tuscia, Dipartimento DECOS, Viterbo, Italy (literal)
Titolo
  • Frictional dissipation at the interface of a two-layer quasi-geostrophic flow (literal)
Abstract
  • In two-layer ocean circulation models the possible dissipation mechanism arising at the interface between the layers is parameterised in terms of the difference between the horizontal velocities of the flow in each layer. We explain and derive such parameterisation by extending the classical Ekman theory, which originally refers to the surface and to the benthic boundary layers, to the interface of a quasi-geostrophic, two-layered flow. (literal)
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