{"refrec":{"BRefID":211186,"RR":"<b>Bozec, Y.; Thomas, H.; Schiettecatte, L.-S.; Borges, A.V.; Elkalay, K.; de Baar, H.J.W.</b> (2006). Assessment of the processes controlling seasonal variations of dissolved inorganic carbon in the North Sea. <i>Limnol. Oceanogr. 51(6)</i>: 2746-2762","BEntID":203108,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":null,"RefStringPartII":". <i>Limnol. Oceanogr. 51(6)</i>: 2746-2762","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Bozec, Y.; Thomas, H.; Schiettecatte, L.-S.; Borges, A.V.; Elkalay, K.; de Baar, H.J.W.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Bozec, Y. <i>et al.</i>","Englishabstract":"We used a seasonal North Sea data set comprising dissolved inorganic carbon (DIC), partial pressure of CO<sub>2</sub> (pCO<sub>2</sub>)), and inorganic nutrients to assess the abiotic and biological processes governing the monthly variations of DIC. During winter, advection and air-sea exchange of CO<sub>2</sub> control and increase the DIC content in the surface and deeper layers of the northern and central North Sea, with the atmosphere supplying CO<sub>2</sub> on the order of 0.2 mol C m<sup>-2</sup> month<sup>-1</sup> to these areas. From February to July, net community production (NCP) controls the seasonal variations of DIC in the surface waters of the entire North Sea, with a net uptake ranging from 0.5 to 1.4 mol C m<sup>-2</sup> month<sup>-1</sup>. During the August-December period, NCP controls the seasonal variations of DIC in the southern North Sea, with a net release ranging from 0.5 to 0.8 mol C m<sup>-2</sup> month<sup>-1</sup>. Similarly, during the April-August period in the deeper layer of the northern North Sea, the NCP was the main factor controlling DIC concentrations, with a net release ranging from 0.5 to 5.5 mol C m<sup>-2</sup> month<sup>-1</sup>. In the surface layer of the North Sea, NCP on the basis of DIC was 4.3 +/- 0.4 mol C m<sup>-2</sup> yr<sup>-1</sup>, whereas, NCP on the basis of nitrate was 1.6 +/- 0.2 mol C m<sup>-2</sup> yr<sup>-1</sup>. Under nutrient-depleted conditions, preferential recycling (extracellular) of nutrients and intracellular mechanisms occurred and were responsible for the non-Redfield uptake of DIC versus nitrate and phosphate.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Assessment of the processes controlling seasonal variations of dissolved inorganic carbon in the North Sea","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:01.897972","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2006,"MonPub":null,"DateUpdate":"2012-01-24","DateCreate":"2011-12-22","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000242265700021","VABBcode":null,"OpenAcc":0},"refs":null,"anarec":{"AnaID":211186,"PubliDate":2006,"Pagination":"2746-2762","XtraPublOfAnaID":null,"ISBN":null,"Volume":"51","Issue":"6","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43511,"SerRR":"Limnology and Oceanography. 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