{"refrec":{"BRefID":251480,"RR":"<b>Bahr, A.; Kaboth, S.; Jiménez-Espejo, F; Sierro, F.J.; Voelker, A.; Lourens, H.L.; Roehl, U.; Reichart, G.J.; Escutia, C.; Hernandez-Molina, F.J.; Pross, J.; Friedrich, O.</b> (2015). Persistent monsoonal forcing of Mediterranean Outflow Water dynamics during the late Pleistocene. <i>Geology (Boulder Colo.) 43(11)</i>: 951-954. <a href=\"http://dx.doi.org/10.1130/G37013.1\" target=\"_blank\">dx.doi.org/10.1130/G37013.1</a>","BEntID":243175,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Geology (Boulder Colo.) 43(11)</i>: 951-954. <a href=\"https://dx.doi.org/10.1130/G37013.1\" target=\"_blank\">https://dx.doi.org/10.1130/G37013.1</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Bahr, A.; Kaboth, S.; Jiménez-Espejo, F; Sierro, F.J.; Voelker, A.; Lourens, H.L.; Roehl, U.; Reichart, G.J.; Escutia, C.; Hernandez-Molina, F.J.; Pross, J.; Friedrich, O.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Bahr, A. <i>et al.</i>","Englishabstract":"The mode and vigor of the global oceanic circulation critically dependon the salinity of (sub)surface water masses advected to the lociof deep-water formation. Within the Atlantic meridional overturningcirculation (AMOC), an important supplier of high-salinity waters isthe Mediterranean Outflow Water (MOW), discharging into the NorthAtlantic via the Strait of Gibraltar. Despite its importance for the NorthAtlantic salinity budget, the long-term dynamics of MOW productionhave remained poorly understood. Here we present high-resolution recordsof bottom-current velocity from three drill sites within the Gulfof Cádiz that document a persistent low-latitude forcing of MOW flowspeed over the past ~150 k.y. We demonstrate that the African monsoonis the predominant driver of orbital-scale MOW variability via itsinfluence on the freshwater budget of the eastern Mediterranean Sea.Consequently, MOW formation fluctuates in concert with orbital precessionoverprinted by centennial-scale oscillations of high-latitude origin.We further document that Northern Hemisphere summer insolationminima stimulate maximal injection of MOW-derived salt into theNorth Atlantic, likely strengthening the intermediate AMOC branch.The direct coupling of MOW dynamics to low-latitude climate forcingrepresents a hitherto neglected process for propagating (sub)tropicalclimate signals into the high northern latitudes.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Persistent monsoonal forcing of Mediterranean Outflow Water dynamics during the late Pleistocene","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2015,"MonPub":null,"DateUpdate":"2015-11-27","DateCreate":"2015-11-27","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000364057700006","VABBcode":null,"OpenAcc":0,"DOI":"10.1130/G37013.1"},"refs":null,"anarec":{"AnaID":251480,"PubliDate":2015,"Pagination":"951-954","XtraPublOfAnaID":null,"ISBN":null,"Volume":"43","Issue":"11","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":42917,"SerRR":"Geology. 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