{"refrec":{"BRefID":210793,"RR":"<b>Keir, R.S.; Rehder, G.; Frankignoulle, M.</b> (2001). Partial pressure and air-sea flux of CO<sub>2</sub> in the Northeast Atlantic during September 1995. <i>Deep-Sea Res., Part 2, Top. Stud. Oceanogr. 48(14-15)</i>: 3179-3189. <a href=\"http://dx.doi.org/10.1016/S0967-0645(01)00036-4\" target=\"_blank\">dx.doi.org/10.1016/S0967-0645(01)00036-4</a>","BEntID":202715,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Deep-Sea Res., Part II, Top. Stud. Oceanogr. 48(14-15)</i>: 3179-3189. <a href=\"https://dx.doi.org/10.1016/S0967-0645(01)00036-4\" target=\"_blank\">https://dx.doi.org/10.1016/S0967-0645(01)00036-4</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Keir, R.S.; Rehder, G.; Frankignoulle, M.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Keir, R.S. <i>et al.</i>","Englishabstract":"Previous work has shown that during early summer, the partial pressure of CO<sub>2</sub> (pCO<sub>2</sub>) in surface waters north of about 45°N in the Atlantic exhibits widespread undersaturation. In many areas. this follows after a \"spring bloom\" of phytoplankton, at which time, nutrient concentrations and pCO<sub>2</sub> decrease sharply from their winter surface values. As part of OMEX I, the late summer distribution of surface water pCO<sub>2</sub> was surveyed in the northeastern Atlantic on cruises of R/V Poseidon and R/V Belgica in 1995. The pattern of the surface distribution of the sea-air pCO<sub>2</sub> difference (Delta pCO<sub>2</sub>) measured on these ship surveys was generally in accord with that observed in this area in early to mid-summer of 1981. The greatest CO<sub>2</sub> undersaturation (-95 µatm) during our surveys was observed near the west coast of Iceland, with Delta pCO<sub>2</sub> increasing to about -60 µatm away from the coast. In shelf waters south of Ireland, the pCO<sub>2</sub> was relatively higher than in surface waters of the open ocean adjacent to the Celtic Shelf margin, but the Celtic Shelf waters were still undersaturated relative to the atmospheric CO<sub>2</sub> concentration. Because of the variation of wind speed, the synoptic distribution of air-sea CO<sub>2</sub> flux, derived from the transfer velocity and Delta pCO<sub>2</sub>, does not resemble the distribution of Delta pCO<sub>2</sub> itself. The sharp increase in wind speed at about 53°N, 20°W during the R/V Poseidon survey produces an order of magnitude rise in the estimated air-sea flux of CO<sub>2</sub>, to a level of about 10-14 mol m<sup>-2</sup> a<sup>-1</sup>. The overall synoptic picture appears to be one of moving centers of higher air-sea fluxes that occur where storms pass over regions of surface water pCO<sub>2</sub> undersaturation.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Partial pressure and air-sea flux of CO<sub>2</sub> in the Northeast Atlantic during September 1995","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2001,"MonPub":null,"DateUpdate":"2012-02-01","DateCreate":"2011-12-22","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000171000700008","VABBcode":null,"OpenAcc":0,"DOI":"10.1016/S0967-0645(01)00036-4"},"refs":null,"anarec":{"AnaID":210793,"PubliDate":2001,"Pagination":"3179-3189","XtraPublOfAnaID":null,"ISBN":null,"Volume":"48","Issue":"14-15","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":45197,"SerRR":"Deep-Sea Research, Part II. 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