Persistent monsoonal forcing of Mediterranean Outflow dynamics during the late Pleistocene, supplement to: Bahr, André; Kaboth, Stefanie; Jiménez-Espejo, Francisco J; Sierro, Francisco Javier; Voelker, Antje H L; Lourens, Lucas Joost; Röhl, Ursula; Reichart, Gert-Jan; Escutia, Carlota; Hernandéz-Molina, Francisco Javier; Pross, Jörg; Friedrich, Oliver (2015): Persistent monsoonal forcing of Mediterranean Outflow Water dynamics during the late Pleistocene. Geology, 43(11), 951-954

André Bahr, Stefanie Kaboth, Francisco J Jiménez-Espejo, Francisco Javier Sierro, Antje H L Voelker, Lucas Joost Lourens, Ursula Röhl, Gert-Jan Reichart, Carlota Escutia, Francisco Javier Hernandéz-Molina, Jörg Pross & Oliver Friedrich
The mode and vigor of the global oceanic circulation critically depend on the salinity of (sub)surface water masses advected to the loci of deep-water formation. Within the Atlantic meridional overturning circulation (AMOC), an important supplier of high-salinity waters is the Mediterranean Outflow Water (MOW), discharging into the North Atlantic via the Strait of Gibraltar. Despite its importance for the North Atlantic salinity budget, the long-term dynamics of MOW production have remained poorly understood. Here we...
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