{"refrec":{"BRefID":302012,"RR":"<b>Claret, M.; Galbraith, E.D.; Palter, J.B.; Bianchi, D.; Fennel, K.; Gilbert, D.; Dunne, J.P.</b> (2018). Rapid coastal deoxygenation due to ocean circulation shift in the northwest Atlantic. <i>Nat. Clim. Chang. 8(10)</i>: 868-872. <a href=\"https://dx.doi.org/10.1038/s41558-018-0263-1\" target=\"_blank\">https://dx.doi.org/10.1038/s41558-018-0263-1</a>","BEntID":294253,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nat. Clim. Chang. 8(10)</i>: 868-872. <a href=\"https://dx.doi.org/10.1038/s41558-018-0263-1\" target=\"_blank\">https://dx.doi.org/10.1038/s41558-018-0263-1</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Claret, M.; Galbraith, E.D.; Palter, J.B.; Bianchi, D.; Fennel, K.; Gilbert, D.; Dunne, J.P.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Claret, M. <i>et al.</i>","Englishabstract":"Global observations show that the ocean lost approximately 2% of its oxygen inventory over the past five decades with important implications for marine ecosystems. The rate of change varies regionally, with northwest Atlantic coastal waters showing a long-term drop that vastly outpaces the global and North Atlantic basin mean deoxygenation rates. However, past work has been unable to differentiate the role of large-scale climate forcing from that of local processes. Here, we use hydrographic evidence to show that a Labrador Current retreat is playing a key role in the deoxygenation on the northwest Atlantic shelf. A high-resolution global coupled climate–biogeochemistry model reproduces the observed decline of saturation oxygen concentrations in the region, driven by a retreat of the equatorward-flowing Labrador Current and an associated shift towards more oxygen-poor subtropical waters on the shelf. The dynamical changes underlying the shift in shelf water properties are correlated with a slowdown in the simulated Atlantic Meridional Overturning Circulation (AMOC). Our results provide strong evidence that a major, centennial-scale change of the Labrador Current is underway, and highlight the potential for ocean dynamics to impact coastal deoxygenation over the coming century.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Rapid coastal deoxygenation due to ocean circulation shift in the northwest Atlantic","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-04 01:31:29.010661","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2018,"MonPub":null,"DateUpdate":"2018-10-12","DateCreate":"2018-10-12","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000445927700016","VABBcode":null,"OpenAcc":0,"DOI":"10.1038/s41558-018-0263-1"},"refs":null,"anarec":{"AnaID":302012,"PubliDate":2018,"Pagination":"868-872","XtraPublOfAnaID":null,"ISBN":null,"Volume":"8","Issue":"10","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":218223,"SerRR":"Nature Climate Change. 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