{"refrec":{"BRefID":318161,"RR":"<b>Wille, J.D.; Favier, V.; Dufour, A.; Gorodetskaya, I.V.; Turner, J.; Agosta, C.; Codron, F.</b> (2019). West Antarctic surface melt triggered by atmospheric rivers. <i>Nature Geoscience 12(11)</i>: 911-916. <a href=\"https://dx.doi.org/10.1038/s41561-019-0460-1\" target=\"_blank\">https://dx.doi.org/10.1038/s41561-019-0460-1</a>","BEntID":311598,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nature Geoscience 12(11)</i>: 911-916. <a href=\"https://dx.doi.org/10.1038/s41561-019-0460-1\" target=\"_blank\">https://dx.doi.org/10.1038/s41561-019-0460-1</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Wille, J.D.; Favier, V.; Dufour, A.; Gorodetskaya, I.V.; Turner, J.; Agosta, C.; Codron, F.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Wille, J.D. <i>et al.</i>","Englishabstract":"Recent major melting events in West Antarctica have raised concerns about a potential hydrofracturing and ice shelf instability. These events often share common forcings of surface melt-like anomalous radiative fluxes, turbulent heat fluxes and föhn winds. Using an atmospheric river detection algorithm developed for Antarctica together with surface melt datasets, we produced a climatology of atmospheric river-related surface melting around Antarctica and show that atmospheric rivers are associated with a large percentage of these surface melt events. Despite their rarity (around 12 events per year in West Antarctica), atmospheric rivers are associated with around 40% of the total summer meltwater generated across the Ross Ice Shelf to nearly 100% in the higher elevation Marie Byrd Land and 40–80% of the total winter meltwater generated on the Wilkins, Bach, George IV and Larsen B and C ice shelves. These events were all related to high-pressure blocking ridges that directed anomalous poleward moisture transport towards the continent. Major melt events in the West Antarctic Ice Sheet only occur about a couple times per decade, but a 1–2 °C warming and continued increase in atmospheric river activity could increase the melt frequency with consequences for ice shelf stability.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"West Antarctic surface melt triggered by atmospheric rivers","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2019,"MonPub":null,"DateUpdate":"2019-11-21","DateCreate":"2019-11-21","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000493905700012","VABBcode":null,"OpenAcc":0,"DOI":"10.1038/s41561-019-0460-1"},"refs":null,"anarec":{"AnaID":318161,"PubliDate":2019,"Pagination":"911-916","XtraPublOfAnaID":null,"ISBN":null,"Volume":"12","Issue":"11","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":123796,"SerRR":"Nature Geoscience. 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