{"refrec":{"BRefID":330030,"RR":"<b>Guarino, M.-V.; Sime, L.C.; Schroeder, D.; Malmierca-Vallet, I.; Rosenblum, E.; Ringer, M.; Ridley, J.; Feltham, D.; Bitz, C.; Steig, E.J.; Wolff, E.; Stroeve, J.; Sellar, A.</b> (2020). Sea-ice-free Arctic during the Last Interglacial supports fast future loss. <i>Nat. Clim. Chang. 10(10)</i>: 928-932. <a href=\"https://dx.doi.org/10.1038/s41558-020-0865-2\" target=\"_blank\">https://dx.doi.org/10.1038/s41558-020-0865-2</a>","BEntID":323637,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nat. Clim. Chang. 10(10)</i>: 928-932. <a href=\"https://dx.doi.org/10.1038/s41558-020-0865-2\" target=\"_blank\">https://dx.doi.org/10.1038/s41558-020-0865-2</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Guarino, M.-V.; Sime, L.C.; Schroeder, D.; Malmierca-Vallet, I.; Rosenblum, E.; Ringer, M.; Ridley, J.; Feltham, D.; Bitz, C.; Steig, E.J.; Wolff, E.; Stroeve, J.; Sellar, A.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Guarino, M.-V. <i>et al.</i>","Englishabstract":"The Last Interglacial (LIG), a warmer period 130,000–116,000 years before present, is a potential analogue for future climate change. Stronger LIG summertime insolation at high northern latitudes drove Arctic land summer temperatures 4–5 °C higher than in the pre-industrial era. Climate model simulations have previously failed to capture these elevated temperatures, possibly because they were unable to correctly capture LIG sea-ice changes. Here, we show that the latest version of the fully coupled UK Hadley Center climate model (HadGEM3) simulates a more accurate Arctic LIG climate, including elevated temperatures. Improved model physics, including a sophisticated sea-ice melt-pond scheme, result in a complete simulated loss of Arctic sea ice in summer during the LIG, which has yet to be simulated in past generations of models. This ice-free Arctic yields a compelling solution to the long-standing puzzle of what drove LIG Arctic warmth and supports a fast retreat of future Arctic summer sea ice.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Sea-ice-free Arctic during the Last Interglacial supports fast future loss","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-15 01:33:26.225379","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2020,"MonPub":null,"DateUpdate":"2020-10-08","DateCreate":"2020-10-08","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000558132800002","VABBcode":null,"OpenAcc":0,"DOI":"10.1038/s41558-020-0865-2"},"refs":null,"anarec":{"AnaID":330030,"PubliDate":2020,"Pagination":"928-932","XtraPublOfAnaID":null,"ISBN":null,"Volume":"10","Issue":"10","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":218223,"SerRR":"Nature Climate Change. 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