{"refrec":{"BRefID":70182,"RR":"<b>Borges, A.V.; Frankignoulle, M.</b> (2003). Distribution of surface carbon dioxide and air-sea exchange in the English Channel and adjacent areas. <i>J. Geophys. Res. 108(C3140)</i>: 14 pp. <a href=\"http://dx.doi.org/10.1029/2000JC000571\" target=\"_blank\">dx.doi.org/10.1029/2000JC000571</a>","BEntID":66237,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>J. Geophys. Res. 108(C3140)</i>: 14 pp. <a href=\"https://dx.doi.org/10.1029/2000JC000571\" target=\"_blank\">https://dx.doi.org/10.1029/2000JC000571</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Borges, A.V.; Frankignoulle, M.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Borges, A.V.; Frankignoulle, M.","Englishabstract":"In the present paper we report the distribution of the partial pressure of CO<sub>2</sub> (<i>p</i>CO<sub>2</sub>) in surface waters along 13 transects in the English Channel, covering the four seasons. The spatial and temporal variability of <i>p</i>CO<sub>2</sub> is controlled by a complex combination of primary production (from May to June), degradation of organic matter, temperature change, and freshwater inputs. Preliminary air-sea CO<sub>2</sub> exchange computations suggest that the Channel is not a major sink of atmospheric CO<sub>2</sub> and is probably neutral from the point of view of atmospheric coupling. 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