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The western branch is capped by a low salinity layer, the origin of which appears to be a mixture of continental shelf water with surface water from the Brazil Current. South of the western branch are two warm-core eddies. These modified warm-core eddies may not re-coalesce with the main thermocline and hence represent a significant salt flux into the subantarctic zone of the South Atlantic.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Brazil-Malvinas Confluence -- 1984","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2025-07-02 08:33:14.980000","timezone_type":1,"timezone":"+00:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":1989,"MonPub":null,"DateUpdate":"2005-11-03","DateCreate":"2005-11-03","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:A1989U266200002","VABBcode":null,"OpenAcc":0},"refs":null,"anarec":{"AnaID":77533,"PubliDate":1989,"Pagination":"359-384","XtraPublOfAnaID":null,"ISBN":null,"Volume":"36","Issue":"3","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":45506,"SerRR":"Deep-Sea Research, Part I. 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