{"refrec":{"BRefID":438074,"RR":"<b>Hoffman, A.O.</b> (2026). Melt channelization stronger than previously recognized. <i>Nat. Clim. Chang. 16(3)</i>: 247-248. <a href=\"https://dx.doi.org/10.1038/s41558-026-02568-2\" target=\"_blank\">https://dx.doi.org/10.1038/s41558-026-02568-2</a>","BEntID":435905,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nat. Clim. Chang. 16(3)</i>: 247-248. <a href=\"https://dx.doi.org/10.1038/s41558-026-02568-2\" target=\"_blank\">https://dx.doi.org/10.1038/s41558-026-02568-2</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Hoffman, A.O.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Hoffman, A.O.","Englishabstract":"Melting beneath floating Antarctic ice shelves is a major driver of ice-shelf mass loss and is projected to increase over the coming century. 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