{"refrec":{"BRefID":338936,"RR":"<b>Findlay, A.</b> (2021). Going way back. <i>Nat. Clim. Chang. 11(6)</i>: 466-466. <a href=\"https://hdl.handle.net/10.1038/s41558-021-01079-6\" target=\"_blank\">https://hdl.handle.net/10.1038/s41558-021-01079-6</a>","BEntID":335571,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nat. Clim. Chang. 11(6)</i>: 466-466. <a href=\"https://hdl.handle.net/10.1038/s41558-021-01079-6\" target=\"_blank\">https://hdl.handle.net/10.1038/s41558-021-01079-6</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Findlay, A.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Findlay, A.","Englishabstract":"The Arctic is warming twice as fast as the rest of the Earth, changing the landscape. In particular, rising temperatures accelerate permafrost thaw, with implications for the vast stores of carbon currently frozen in these soils. 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