The Western Mediterranean Deep Water: A proxy for climate change - art. no. L12608

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).

Keyword(s)

North Atlantic, West mediterranee, Thermohaline circulation, Temperature variation, Deep water, Water masses, Air sea heat flux

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Rixen Michel, Beckers J, Levitus S, Antonov J, Boyer T, Maillard Catherine, Fichaut Michele, Balopoulos E, Iona S, Dooley H, Garcia M, Manca B, Giorgetti A, Manzella G, Mikhailov N, Pinardi N, Zavatarelli M (2005). The Western Mediterranean Deep Water: A proxy for climate change - art. no. L12608. Geophysical Research Letters. 32 (12). NIL_47-NIL_50. https://doi.org/10.1029/2005GL022702, https://archimer.ifremer.fr/doc/00000/760/

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