The Western Mediterranean Deep Water: A proxy for climate change - art. no. L12608
Type | Article | ||||||||
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Date | 2005-06 | ||||||||
Language | English | ||||||||
Author(s) | Rixen Michel1, 2, Beckers J2, Levitus S3, Antonov J3, Boyer T3, Maillard Catherine4, Fichaut Michele![]() |
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Affiliation(s) | 1 : NURC, I-19138 La Spezia, Italy. 2 : Univ Liege, Inst Phys, MARE GHER, B-4000 Liege, Belgium. 3 : NOAA, NODC, Silver Spring, MD 20910 USA. 4 : IFREMER, Ctr Brest, SISMER, F-29280 Plouzane, France. 5 : Aghios Kosmas hellinikon, HNODC, NCMR, Athens 16604, Greece. 6 : ICES, DK-1261 Copenhagen, Denmark. 7 : IEO, Madrid 28002, Spain. 8 : OGS, I-34010 Sgonico, Italy. 9 : ENEA, CRAM, I-19100 La Spezia, Italy. 10 : RIHMI WDC, Obninsk 249020, Kaluga Region, Russia. 11 : Univ Bologna, Dept Phys, Alma Mater Studiorum, I-40127 Bologna, Italy. |
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Source | Geophysical Research Letters (0094-8276) (AGU), 2005-06 , Vol. 32 , N. 12 , P. NIL_47-NIL_50 | ||||||||
DOI | 10.1029/2005GL022702 | ||||||||
WOS© Times Cited | 216 | ||||||||
Keyword(s) | North Atlantic, West mediterranee, Thermohaline circulation, Temperature variation, Deep water, Water masses, Air sea heat flux | ||||||||
Abstract | Reconstructions of Mediterranean ocean temperature fields back to 1950 show a proxy relationship between heat content changes in the North Atlantic and the Western Mediterranean Deep Water ( WMDW) formed in the Gulf of Lions in winter, because of consistent air-sea heat fluxes over these areas, strongly correlated to the North Atlantic Oscillation ( NAO). | ||||||||
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