{"refrec":{"BRefID":382847,"RR":"<b>Kochtitzky, W.; Copland, L.; King, M.; Hugonnet, R.; Jiskoot, H.; Morlighem, M.; Millan, R.; Khan, S.A.; Noël, B.</b> (2023). Closing Greenland's mass balance: frontal ablation of every Greenlandic glacier from 2000 to 2020. <i>Geophys. Res. Lett. 50(17)</i>: e2023GL104095. <a href=\"https://dx.doi.org/10.1029/2023GL104095\" target=\"_blank\">https://dx.doi.org/10.1029/2023GL104095</a>","BEntID":380589,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Geophys. Res. Lett. 50(17)</i>: e2023GL104095. <a href=\"https://dx.doi.org/10.1029/2023GL104095\" target=\"_blank\">https://dx.doi.org/10.1029/2023GL104095</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Kochtitzky, W.; Copland, L.; King, M.; Hugonnet, R.; Jiskoot, H.; Morlighem, M.; Millan, R.; Khan, S.A.; Noël, B.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Kochtitzky, W. <i>et al.</i>","Englishabstract":"<p style=\"margin-left:0px;\">In Greenland, 87% of the glacierized area terminates in the ocean, but mass lost at the ice-ocean interface, or frontal ablation, has not yet been fully quantified. Using measurements and models we calculate frontal ablation of Greenland's 213 outlet and 537 peripheral glaciers and find a total frontal ablation of 481.8&nbsp;±&nbsp;24.0 for 2000–2010 and 510.2&nbsp;±&nbsp;18.6&nbsp;Gt&nbsp;a<sup>−1</sup> for 2010–2020. Ice discharge accounted for ∼90% of frontal ablation during both periods, while mass loss due to terminus retreat comprised the remainder. Only 16 glaciers were responsible for the majority (&gt;50%) of frontal ablation from 2010 to 2020. These estimates, along with the climatic-basal balance, allow for a more complete accounting of Greenland Ice Sheet and peripheral glacier mass balance. In total, Greenland accounted for ∼90% of Northern Hemisphere frontal ablation for 2000–2010 and 2010–2020.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Closing Greenland's mass balance: frontal ablation of every Greenlandic glacier from 2000 to 2020","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-04-18 01:32:42.992264","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"glaciology; remote sensing; frontal ablation; glacier mass loss; cryosphere; calving","OtherDescriptors":null,"Notes":null,"AnaPub":2023,"MonPub":null,"DateUpdate":"2024-02-26","DateCreate":"2024-02-16","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:001063240000001","VABBcode":null,"OpenAcc":1,"DOI":"10.1029/2023GL104095"},"refs":null,"anarec":{"AnaID":382847,"PubliDate":2023,"Pagination":"e2023GL104095","XtraPublOfAnaID":null,"ISBN":null,"Volume":"50","Issue":"17","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":42920,"SerRR":"Geophysical Research Letters. 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