Seasonal variability of the mixed layer depth in the Mediterranean Sea as derived from in situ profiles (Articolo in rivista)

Type

• Articolo in rivista (Classe)
• Prodotto della ricerca (Classe)

Label

• Seasonal variability of the mixed layer depth in the Mediterranean Sea as derived from in situ profiles (Articolo in rivista) (literal)

Anno

• 2005-01-01T00:00:00+01:00 (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi

• 10.1029/2005GL022463 (literal)

Alternative label

• F. D'’Ortenzio (1); D. Iudicone (2); C. de Boyer Montegut (3); P. Testor (4); D. Antoine (1); S. Marullo (5); R. Santoleri (6); G. Madec (3) (2005)
  Seasonal variability of the mixed layer depth in the Mediterranean Sea as derived from in situ profiles
  in Geophysical research letters
  (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori

• F. D'’Ortenzio (1); D. Iudicone (2); C. de Boyer Montegut (3); P. Testor (4); D. Antoine (1); S. Marullo (5); R. Santoleri (6); G. Madec (3) (literal)

Pagina inizio

• L12605-1 (literal)

Pagina fine

• L12605-4 (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume

• 32 (literal)

Rivista

• Geophysical research letters (Rivista)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroFascicolo

• 12 (literal)

Note

• ISI Web of Science (WOS) (literal)
• Scopu (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni

• 1 Laboratoire d'Oceanographie de Villefranche, Villefranche-sur-mer,France. 2 Stazione Zoologica Napoli, Naples, Italy. 3 Laboratoire d'Oceanographie Dynamique et de Climatologie, Paris,France. 4 Leibniz-Institut fu¨ r Meereswissenschaften, Kiel, Germany. 5 Centro Ricerche Frascati, Ente per le Nuove Tecnologie, l'Energia el'Ambiente, Frascati, Italy. 6 Istituto Scienze Atmosfera e Clima, Rome, Italy. (literal)

Titolo

• Seasonal variability of the mixed layer depth in the Mediterranean Sea as derived from in situ profiles (literal)

Abstract

• A new 0.5 resolution Mediterranean climatology of the mixed layer depth based on individual profiles of temperature and salinity has been constructed. The criterion selected is a threshold value of temperature from a near-surface value at 10 m depth, mainly derived by a method applied on the global (de Boyer Montégut et al., 2004 dBM04). With respect to dBM04, the main differences reside in the absence of spatial interpolation of the final fields and in the improved spatial resolution. These changes to the method are necessary to reproduce the Mediterranean mixed layer's behavior. In the derived climatological maps, the most relevant features of the basin surface circulation are reproduced, as well as the areas prone of the deep water formation are clearly identified. Finally, the role of density in the definition of the mixed layer's differing behaviors between the oriental and the occidental regions of the basin is presented. (literal)

Prodotto di

• dinamica marina e produttività biologica da misure satellitari (TA.P04.017.003) (Modulo)
• Institute of atmospheric sciences and climate (ISAC) (Istituto)

Autore CNR

• ROSALIA SANTOLERI (Unità di personale interno)

Incoming links:

Prodotto

• Institute of atmospheric sciences and climate (ISAC) (Istituto)
• dinamica marina e produttività biologica da misure satellitari (TA.P04.017.003) (Modulo)

Autore CNR di

• ROSALIA SANTOLERI (Unità di personale interno)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#rivistaDi

• Geophysical research letters (Rivista)