{"refrec":{"BRefID":349097,"RR":"<b>Findlay, A.</b> (2022). From under the ice. <i>Nat. Clim. Chang. 12(1)</i>: 7. <a href=\"https://dx.doi.org/10.1038/s41558-021-01257-6\" target=\"_blank\">https://dx.doi.org/10.1038/s41558-021-01257-6</a>","BEntID":346792,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nat. Clim. Chang. 12(1)</i>: 7. <a href=\"https://dx.doi.org/10.1038/s41558-021-01257-6\" target=\"_blank\">https://dx.doi.org/10.1038/s41558-021-01257-6</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 rapidly, and thawing peatlands and permafrost are a potentially large source of GHG emissions to the atmosphere as frozen carbon is remobilized. 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