Vertical distribution of dissolved organic carbon (DOC) in the Western Mediterranean Sea in relation to the hydrological characteristics (Articolo in rivista)

Type
Label
  • Vertical distribution of dissolved organic carbon (DOC) in the Western Mediterranean Sea in relation to the hydrological characteristics (Articolo in rivista) (literal)
Anno
  • 2002-01-01T00:00:00+01:00 (literal)
Alternative label
  • Santinelli C., Gasparini G.P., Nannicini L., Seritti A. (2002)
    Vertical distribution of dissolved organic carbon (DOC) in the Western Mediterranean Sea in relation to the hydrological characteristics
    in Deep-sea research. Part 1. Oceanographic research papers
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • Santinelli C., Gasparini G.P., Nannicini L., Seritti A. (literal)
Pagina inizio
  • 2203 (literal)
Pagina fine
  • 2219 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
  • 49 (literal)
Rivista
Note
  • ISI Web of Science (WOS) (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • Istituto di Biofisica (literal)
Titolo
  • Vertical distribution of dissolved organic carbon (DOC) in the Western Mediterranean Sea in relation to the hydrological characteristics (literal)
Abstract
  • Vertical profiles of dissolved organic carbon (DOC) from eight hydrological stations in the Thyrrhenian Sea, Sardinia Channel and Algerian Sea, are reported. DOC exhibits concentrations ranging from 58 to 88 uM in surface water, 47-57 uM in the intermediate layer and 49-63 uM in deep waters. The assessment of the hydrological characteristics allows different water masses in the study area to be identified; moreover, different hydrological processes are observed in the Tyrrhenian and Algerian basins. DOC exhibits different values in the different water masses. The lowest DOC concentrations (43-46 uM) were found in the Tyrrhenian Levantine Intermediate Water (LIW). Correlations between intermediate and deep waters, suggesting the occurrence of different processes of oxygen consumption in the different water masses. (literal)
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