{"refrec":{"BRefID":353529,"RR":"<b>Stoll, H.M.; Cacho, I.; Gasson, E.; Sliwinski, J.; Kost, O.; Moreno, A.; Iglesias, M.; Torner, J.; Perez-Mejias, C.; Haghipour, N.; Cheng, H.; Edwards, R.L.</b> (2022). Rapid northern hemisphere ice sheet melting during the penultimate deglaciation. <i>Nature Comm. 13(1)</i>: 3819. <a href=\"https://dx.doi.org/10.1038/s41467-022-31619-3\" target=\"_blank\">https://dx.doi.org/10.1038/s41467-022-31619-3</a>","BEntID":351239,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nature Comm. 13(1)</i>: 3819. <a href=\"https://dx.doi.org/10.1038/s41467-022-31619-3\" target=\"_blank\">https://dx.doi.org/10.1038/s41467-022-31619-3</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Stoll, H.M.; Cacho, I.; Gasson, E.; Sliwinski, J.; Kost, O.; Moreno, A.; Iglesias, M.; Torner, J.; Perez-Mejias, C.; Haghipour, N.; Cheng, H.; Edwards, R.L.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Stoll, H.M. <i>et al.</i>","Englishabstract":"The rate and consequences of future high latitude ice sheet retreat remain a major concern given ongoing anthropogenic warming. Here, new precisely dated stalagmite data from NW Iberia provide the first direct, high-resolution records of periods of rapid melting of Northern Hemisphere ice sheets during the penultimate deglaciation. These records reveal the penultimate deglaciation initiated with rapid century-scale meltwater pulses which subsequently trigger abrupt coolings of air temperature in NW Iberia consistent with freshwater-induced AMOC slowdowns. The first of these AMOC slowdowns, 600-year duration, was shorter than Heinrich 1 of the last deglaciation. Although similar insolation forcing initiated the last two deglaciations, the more rapid and sustained rate of freshening in the eastern North Atlantic penultimate deglaciation likely reflects a larger volume of ice stored in the marine-based Eurasian Ice sheet during the penultimate glacial in contrast to the land-based ice sheet on North America as during the last glacial.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Rapid northern hemisphere ice sheet melting during the penultimate deglaciation","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-05-30 01:32:00.279643","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2022,"MonPub":null,"DateUpdate":"2022-07-07","DateCreate":"2022-07-07","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000820356400020","VABBcode":null,"OpenAcc":1,"DOI":"10.1038/s41467-022-31619-3"},"refs":null,"anarec":{"AnaID":353529,"PubliDate":2022,"Pagination":"3819","XtraPublOfAnaID":null,"ISBN":null,"Volume":"13","Issue":"1","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":198717,"SerRR":"Nature Communications. 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