{"refrec":{"BRefID":363277,"RR":"(2023). Winter sea-ice growth in the Arctic impeded by more frequent atmospheric rivers. <i>Nat. Clim. Chang. 13(3)</i>: 222-223. <a href=\"https://dx.doi.org/10.1038/s41558-023-01601-y\" target=\"_blank\">https://dx.doi.org/10.1038/s41558-023-01601-y</a>","BEntID":360995,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nat. Clim. Chang. 13(3)</i>: 222-223. <a href=\"https://dx.doi.org/10.1038/s41558-023-01601-y\" target=\"_blank\">https://dx.doi.org/10.1038/s41558-023-01601-y</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":null,"OrigTitleTranslFlag":0,"Authorstringtrunc":null,"Englishabstract":"Over the past four decades, Arctic sea ice has experienced a drastic decline in winter when it is recovering from summer melt. 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