{"refrec":{"BRefID":337529,"RR":"<b>Sun, S.; Pattyn, F.; Simon, E.G.; Albrecht, T.; Cornford, S.; Calov, R.; Dumas, C.; Gillet-Chaulet, F.; Goelzer, H.; Golledge, N.R.; Greve, R.; Hoffman, M.J.; Humbert, A.; Kazmierczak, E.; Kleiner, T.; Leguy, G.R.; Lipscomb, W.H.; Martin, D.; Morlighem, M.; Nowicki, S.; Pollard, D.; Price, S.; Quiquet, A.; Seroussi, H.; Schlemm, T.; Sutter, J.; van de Wal, R.S.W; Winkelmann, R.; Zhang, T.</b> (2020). Antarctic ice sheet response to sudden and sustained ice-shelf collapse (ABUMIP). <i>J. Glaciol. 66(260)</i>: 891-904. <a href=\"https://hdl.handle.net/10.1017/jog.2020.67\" target=\"_blank\">https://hdl.handle.net/10.1017/jog.2020.67</a>","BEntID":334152,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>J. Glaciol. 66(260)</i>: 891-904. <a href=\"https://hdl.handle.net/10.1017/jog.2020.67\" target=\"_blank\">https://hdl.handle.net/10.1017/jog.2020.67</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Sun, S.; Pattyn, F.; Simon, E.G.; Albrecht, T.; Cornford, S.; Calov, R.; Dumas, C.; Gillet-Chaulet, F.; Goelzer, H.; Golledge, N.R.; Greve, R.; Hoffman, M.J.; Humbert, A.; Kazmierczak, E.; Kleiner, T.; Leguy, G.R.; Lipscomb, W.H.; Martin, D.; Morlighem, M.; Nowicki, S.; Pollard, D.; Price, S.; Quiquet, A.; Seroussi, H.; Schlemm, T.; Sutter, J.; van de Wal, R.S.W; Winkelmann, R.; Zhang, T.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Sun, S. <i>et al.</i>","Englishabstract":"Antarctica's ice shelves modulate the grounded ice flow, and weakening of ice shelves due to climate forcing will decrease their ‘buttressing’ effect, causing a response in the grounded ice. While the processes governing ice-shelf weakening are complex, uncertainties in the response of the grounded ice sheet are also difficult to assess. The Antarctic BUttressing Model Intercomparison Project (ABUMIP) compares ice-sheet model responses to decrease in buttressing by investigating the ‘end-member’ scenario of total and sustained loss of ice shelves. Although unrealistic, this scenario enables gauging the sensitivity of an ensemble of 15 ice-sheet models to a total loss of buttressing, hence exhibiting the full potential of marine ice-sheet instability. All models predict that this scenario leads to multi-metre (1–12 m) sea-level rise over 500 years from present day. West Antarctic ice sheet collapse alone leads to a 1.91–5.08 m sea-level rise due to the marine ice-sheet instability. Mass loss rates are a strong function of the sliding/friction law, with plastic laws cause a further destabilization of the Aurora and Wilkes Subglacial Basins, East Antarctica. Improvements to marine ice-sheet models have greatly reduced variability between modelled ice-sheet responses to extreme ice-shelf loss, e.g. compared to the SeaRISE assessments.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Antarctic ice sheet response to sudden and sustained ice-shelf collapse (ABUMIP)","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-01 01:32:08.597826","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Antarctic glaciology; ice-sheet modelling; ice shelves","OtherDescriptors":null,"Notes":null,"AnaPub":2020,"MonPub":null,"DateUpdate":"2021-05-22","DateCreate":"2021-05-17","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000592212900001","VABBcode":null,"OpenAcc":1,"Handle":"10.1017/jog.2020.67"},"refs":null,"anarec":{"AnaID":337529,"PubliDate":2020,"Pagination":"891-904","XtraPublOfAnaID":null,"ISBN":null,"Volume":"66","Issue":"260","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":219460,"SerRR":"Journal of Glaciology. 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