{"refrec":{"BRefID":249352,"RR":"<b>Moore, G.W.K.; Våge, K.; Pickart, R.S.; Renfrew, I.A.</b> (2015). Decreasing intensity of open-ocean convection in the Greenland and Iceland seas. <i>Nat. Clim. Chang. 5(9)</i>: 877–882. <a href=\"http://dx.doi.org/10.1038/nclimate2688\" target=\"_blank\">http://dx.doi.org/10.1038/nclimate2688</a>","BEntID":241056,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nat. Clim. Chang. 5(9)</i>: 877–882. <a href=\"http://dx.doi.org/10.1038/nclimate2688\" target=\"_blank\">http://dx.doi.org/10.1038/nclimate2688</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Moore, G.W.K.; Våge, K.; Pickart, R.S.; Renfrew, I.A.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Moore, G.W.K. <i>et al.</i>","Englishabstract":"A combination of retreating sea ice and different rates of warming in the Greenland and Iceland seas is reducing winter air–sea heat fluxes. 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