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Intensification and spatial homogenization of coastal upwelling under climate change. <i>Nature (Lond.) 518(7539)</i>: 390–394. <a href=\"http://dx.doi.org/10.1038/nature14235\" target=\"_blank\">http://dx.doi.org/10.1038/nature14235</a>","BEntID":236768,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nature (Lond.) 518(7539)</i>: 390–394. <a href=\"http://dx.doi.org/10.1038/nature14235\" target=\"_blank\">http://dx.doi.org/10.1038/nature14235</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Wang, D.; Gouhier, T.C.; Menge, B.A.; Ganguly, A.R.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Wang, D. <i>et al.</i>","Englishabstract":"An ensemble of climate models shows that by the end of the twenty-first century the coastal upwelling season near the eastern boundaries of the Atlantic and Pacific oceans will start earlier, end later and become more intense at high latitudes, thus becoming more homogeneous; these changes may affect the geographical distribution of marine biodiversity.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Intensification and spatial homogenization of coastal upwelling under climate change","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-08 01:31:00.767344","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2015,"MonPub":null,"DateUpdate":"2018-02-13","DateCreate":"2015-02-24","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000349547400040","VABBcode":null,"OpenAcc":0,"DOI":"10.1038/nature14235"},"refs":null,"anarec":{"AnaID":245083,"PubliDate":2015,"Pagination":"390–394","XtraPublOfAnaID":null,"ISBN":null,"Volume":"518","Issue":"7539","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43431,"SerRR":"Nature: International Weekly Journal of Science. 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