The Western Mediterranean Deep Water: A proxy for climate change

Details The Western Mediterranean Deep Water: A proxy for climate change The Western Mediterranean Deep Water: A proxy for climate change

Jun 2005

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2005georl..3212608r&link_type=abstract

Geophysical Research Letters, Volume 32, Issue 12, CiteID L12608

Physics

42

Global Change: Climate Variability (1635, 3305, 3309, 4215, 4513), Oceanography: General: Climate And Interannual Variability (1616, 1635, 3305, 3309, 4513), Global Change: Regional Climate Change

Scientific paper

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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