Pregled bibliografske jedinice broj: 618277
Winter convection continues in the warming Southern Adriatic
Winter convection continues in the warming Southern Adriatic // Eos (Washington, D.C.), 86 (2005), 45; 451-455 doi:10.1029/2005EO450002 (međunarodna recenzija, članak, znanstveni)
CROSBI ID: 618277 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Winter convection continues in the warming Southern Adriatic
Autori
Civitarese, G. ; Gačić, Miroslav ; Cardin, V. ; Ibello, V.
Izvornik
Eos (Washington, D.C.) (0096-3941) 86
(2005), 45;
451-455
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Sažetak
During winters in the eastern Mediterranean, cold winds blow over the waters of the southern portion of the Adriatic Sea, resulting in heat loss of the ocean. This cold surface water becomes denser than surrounding waters and sinks into the deep reaches of the Mediterranean Sea. This forms ‘deep water, ’ or water once at the ocean's surface that now has sunk to depths of 1500 meters and more. The Southern Adriatic Pit (SAP) is the convection site and source for the Eastern Mediterranean Deep Water (EMDW). Since the late 1980s, the SAP has been monitored almost every year because of its importance in driving the eastern Mediterranean deep circulation convection cell.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
Citiraj ovu publikaciju:
Časopis indeksira:
- Scopus
