The Seasonal and Interannual Variability in the Ligurian-Povencal Basin (Contributo in volume (capitolo o saggio))

Type
Label
  • The Seasonal and Interannual Variability in the Ligurian-Povencal Basin (Contributo in volume (capitolo o saggio)) (literal)
Anno
  • 1994-01-01T00:00:00+01:00 (literal)
Alternative label
  • M. Astraldi, G.P. Gasparini, S. Sparnocchia (1994)
    The Seasonal and Interannual Variability in the Ligurian-Povencal Basin
    AGU, American geophysical union, Washington, DC (Stati Uniti d'America) in Seasonal and Interannual Variability of the Western Mediterranean Sea, 1994
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • M. Astraldi, G.P. Gasparini, S. Sparnocchia (literal)
Pagina inizio
  • 93 (literal)
Pagina fine
  • 113 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#url
  • http://www.agu.org/books/ce/v046/ (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#titoloVolume
  • Seasonal and Interannual Variability of the Western Mediterranean Sea (literal)
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  • 46 (literal)
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  • 21 (literal)
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  • CNR-Stazione Oceanografica, Pozzuolo di Lerici (SP) (literal)
Titolo
  • The Seasonal and Interannual Variability in the Ligurian-Povencal Basin (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#isbn
  • 0-87590-260-X (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autoriVolume
  • P. E. La Viollette (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#curatoriVolume
  • P. E. La Viollette (literal)
Abstract
  • The circulation characteristics of the Ligurian-Provençal Basin are examined for the purpose of evaluating the possible forcings and the principal oscillations of the basin circulation. A critical review of the literature and available data (including model- simulation) indicates that the atmospheric-climatic conditions in winter are the principal factor conditioning the basin circulation. According to the field observations, these conditions generate different thermohaline properties in the Ligurian-Provençal Basin and the adjacent Tyrrhenian Sea. The gradient thus generated induces a winter outflow of warmer Tyrrhenian water through the Corsica Channel and then a seasonal oscillation of the Ligurian-Provençal Current. Though less evident, another seasonal oscillation seems to be present in the Ligurian-Provençal current system. This is visible along the western side of Corsica where it is shown as a progressive increase of the current velocity that reaches a maximum in early summer. This corresponds to the seasonal increase of the current indicated by a numerical model driven by deep water formation. We therefore suggest that this oscillation might represent the signal of the deep water formation on the boundary circulation. (literal)
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