http://www.cnr.it/ontology/cnr/individuo/prodotto/ID45137
On the dynamics of surface cold filaments in the Mediterranean Sea (Articolo in rivista)
- Type
- Label
- On the dynamics of surface cold filaments in the Mediterranean Sea (Articolo in rivista) (literal)
- Anno
- 2008-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1016/j.jmarsys.2008.03.002 (literal)
- Alternative label
Bignami, F; Böhm, E; D'Acunzo, E; R. D'Archino and E. Salusti (2008)
On the dynamics of surface cold filaments in the Mediterranean Sea
in Journal of marine systems
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Bignami, F; Böhm, E; D'Acunzo, E; R. D'Archino and E. Salusti (literal)
- Pagina inizio
- Pagina fine
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- http://www.sciencedirect.com/science/article/pii/S0924796308000547 (literal)
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- ISI Web of Science (WOS) (literal)
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- ISAC - Unit`Organizzativa di Supporto di Roma (literal)
- Titolo
- On the dynamics of surface cold filaments in the Mediterranean Sea (literal)
- Abstract
- Thermal NOAA/AVHRR satellite images relative to the years 1997-2000 are analyzed in this study, in order to obtain a first systematic identification of the sites of highest frequency in cold filaments in the Mediterranean Sea, as well as their properties. These sites are characterised by upwelling and/or the funnelling of strong cold winds by a somewhat irregular coastal orography. Indeed, intense air?sea interaction in the coastal zone generates a particularly strong input of potential vorticity into the sea. This in turn gives origin to cold filaments and jets. In the Mediterranean Sea, the geographical zones with a higher frequency in these jets are the two lobes of the southern Sicilian coast, the sea off eastern Sardinia, that south of the island of Crete, where a particularly intense mesoscale field is evident, and the Balkan coast of the Adriatic Sea. A chosen subset of the examined images is here used to obtain an estimate of a bulk coefficient M for mass exchange between filaments and ambient water, in order to explain the along-flow warming observed in most of the satellite images, at each filament site. (literal)
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