{"refrec":{"BRefID":300649,"RR":"<b>Wake, B.</b> (2018). Regional heat uptake. <i>Nat. Clim. Chang. 8(8)</i>: 662-662. <a href=\"https://dx.doi.org/10.1038/s41558-018-0251-5\" target=\"_blank\">https://dx.doi.org/10.1038/s41558-018-0251-5</a>","BEntID":292886,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nat. Clim. Chang. 8(8)</i>: 662-662. <a href=\"https://dx.doi.org/10.1038/s41558-018-0251-5\" target=\"_blank\">https://dx.doi.org/10.1038/s41558-018-0251-5</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Wake, B.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Wake, B.","Englishabstract":"Much of the global uptake of anthropogenic heat has occurred in the Southern Ocean. Upwelling of cold, deep waters to the surface allows the heat uptake, which is then transported northwards through the overturning circulation. 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