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The multi-millennial Antarctic commitment to future sea-level rise. <i>Nature (Lond.) 526(7573)</i>: 421–425. <a href=\"http://dx.doi.org/10.1038/nature15706\" target=\"_blank\">http://dx.doi.org/10.1038/nature15706</a>","BEntID":242244,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nature (Lond.) 526(7573)</i>: 421–425. <a href=\"http://dx.doi.org/10.1038/nature15706\" target=\"_blank\">http://dx.doi.org/10.1038/nature15706</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Golledge, N.R.; Kowalewski, D.E.; Naish, T.R.; Levy, R.H.; Fogwill, C.J.; Gasson, E.G.W.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Golledge, N.R. <i>et al.</i>","Englishabstract":"Despite computational and methodological uncertainties, and a wide range of potential greenhouse gas emissions, here millennial-scale simulations of the Antarctic Ice Sheet in a warming climate show that most of Antarctica’s fringing ice shelves will collapse, leading to a rise in sea level of up to 3 metres by 2300.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"The multi-millennial Antarctic commitment to future sea-level rise","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-15 01:32:45.299837","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":"2015-10-16","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000362730200049","VABBcode":null,"OpenAcc":0,"DOI":"10.1038/nature15706"},"refs":null,"anarec":{"AnaID":250550,"PubliDate":2015,"Pagination":"421–425","XtraPublOfAnaID":null,"ISBN":null,"Volume":"526","Issue":"7573","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43431,"SerRR":"Nature: International Weekly Journal of Science. 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