{"refrec":{"BRefID":284413,"RR":"<b>Evans, G.R.; McDonagh, E.L.; King, B.A.; Bryden, H.L.; Bakker, D.C.E.; Brown, P.J.; Schuster, U.; Speer, K.G.; van Heuven, S.M.A.C.</b> (2017). South Atlantic interbasin exchanges of mass, heat, salt and anthropogenic carbon. <i>Prog. Oceanogr. 151</i>: 62-82. <a href=\"http://dx.doi.org/10.1016/j.pocean.2016.11.005\" target=\"_blank\">dx.doi.org/10.1016/j.pocean.2016.11.005</a>","BEntID":276437,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":null,"RefStringPartII":". <i>Prog. Oceanogr. 151</i>: 62-82. <a href=\"https://dx.doi.org/10.1016/j.pocean.2016.11.005\" target=\"_blank\">https://dx.doi.org/10.1016/j.pocean.2016.11.005</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Evans, G.R.; McDonagh, E.L.; King, B.A.; Bryden, H.L.; Bakker, D.C.E.; Brown, P.J.; Schuster, U.; Speer, K.G.; van Heuven, S.M.A.C.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Evans, G.R. <i>et al.</i>","Englishabstract":"The exchange of mass, heat, salt and anthropogenic carbon (Cant) between the South Atlantic, south of 24°S, and adjacent ocean basins is estimated from hydrographic data obtained during 2008–2009 using an inverse method. Transports of anthropogenic carbon are calculated across the western (Drake Passage), eastern (30°E) and northern (24°S) boundaries. The freshwater overturning transport of 0.09 Sv is southward, consistent with an overturning circulation that exports freshwater from the North Atlantic, and consistent with a bistable Meridional Overturning Circulation (MOC), under conditions of excess freshwater perturbation. At 30°E, net eastward Antarctic Circumpolar Current (ACC) transport, south of the Subtropical Front, is compensated by a 15.9 ± 2.3 Sv westward flow along the Antarctic boundary. The region as a whole is a substantial sink for atmospheric anthropogenic carbon of 0.51 ± 0.37 Pg C yr−1, of which 0.18 ± 0.12 Pg C yr−1 accumulates and is stored within the water column. At 24°S, a 20.2 Sv meridional overturning is associated with a 0.11 Pg C yr−1 Cant overturning. The remainder is transported into the Atlantic Ocean north of 24°S (0.28 ± 0.16 Pg C yr−1) and Indian sector of Southern Ocean (1.12 ± 0.43 Pg C yr−1), having been enhanced by inflow through Drake Passage (1.07 ± 0.44 Pg C yr−1). This underlines the importance of the South Atlantic as a crucial element of the anthropogenic carbon sink in the global oceans.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"South Atlantic interbasin exchanges of mass, heat, salt and anthropogenic carbon","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":2017,"MonPub":null,"DateUpdate":"2017-04-13","DateCreate":"2017-04-13","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000395609900005","VABBcode":null,"OpenAcc":0,"DOI":"10.1016/j.pocean.2016.11.005"},"refs":null,"anarec":{"AnaID":284413,"PubliDate":2017,"Pagination":"62-82","XtraPublOfAnaID":null,"ISBN":null,"Volume":"151","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43700,"SerRR":"Progress in Oceanography. 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