{"refrec":{"BRefID":62030,"RR":"<b>Thomas, H.; Bozec, Y.; Elkalay, K.; de Baar, H.J.W.</b> (2004). Enhanced open ocean storage of CO<sub>2</sub> from shelf sea pumping. <i>Science (Wash.) 304(5673)</i>: 1005-1008. <a href=\"https://dx.doi.org/10.1126/science.1095491\" target=\"_blank\">https://dx.doi.org/10.1126/science.1095491</a>","BEntID":58662,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Science (Wash.) 304(5673)</i>: 1005-1008. <a href=\"https://dx.doi.org/10.1126/science.1095491\" target=\"_blank\">https://dx.doi.org/10.1126/science.1095491</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Thomas, H.; Bozec, Y.; Elkalay, K.; de Baar, H.J.W.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Thomas, H. <i>et al.</i>","Englishabstract":"Seasonal field observations show that the North Sea, a Northern European shelf sea, is highly efficient in pumping carbon dioxide from the atmosphere to the North Atlantic Ocean. The bottom topography–controlled stratification separates production and respiration processes in the North Sea, causing a carbon dioxide increase in the subsurface layer that is ultimately exported to the North Atlantic Ocean. 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