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dc.contributor.authorBellerby, Richard G. J.eng
dc.contributor.authorHoppema, M.eng
dc.contributor.authorFahrbach, E.eng
dc.contributor.authorBaar, H. J. W. deeng
dc.contributor.authorStoll, M.eng
dc.date.accessioned2004-07-12T09:22:15Z
dc.date.accessioned2004-08-03T12:58:19Z
dc.date.accessioned2004-08-26T11:57:57Z
dc.date.available2004-07-12T09:22:15Z
dc.date.available2004-08-03T12:58:19Z
dc.date.available2004-08-26T11:57:57Z
dc.date.issued2004-06eng
dc.identifier.citationDeep Sea Research Part I: Oceanographic Research Papers 2004 51(6): 793-808en
dc.identifier.issn0967-0637eng
dc.identifier.urihttp://hdl.handle.net/1956/386
dc.description.abstractThe fugacity of carbon dioxide (fCO2) of the surface waters of the Weddell Sea along the prime meridian has been described for the austral autumn in 1996 and 1998. For individual years, fCO2 has a strong linear relationship with sea surface temperature, although the relationships cannot be reconciled to provide an interannually consistent algorithm for remotely sensed assessment of fCO2: However, from the assumption that Weddell Sea surface water has a single end member (upwelled Warm Deep Water) we have determined the relative contributions of heating, ice-melt, and biological activity on fCO2: A breakdown of the controls shows that the measured annual fCO2 distributions can be recreated for both transects by adjusting solely for thermodynamic forcing, and model adjustments for salinity are small except in regions of significant upwelling during 1998. The incorporation of nitrate utilisation into the model results in a general and significant underestimation of fCO2: This runs contrary to the earlier findings ofSabine and Key (Mar. Chem. 60 (1998) 95) in the Southern Ocean although it is consistent with models in the area (Louanchi et al., Deep-Sea Res. I 48 (2001) 1581). A major caveat to these findings is the significant departure ofthe thermodynamic model and a tightening ofthe nitrate-adjusted model in 1998 in areas with deeper mixing in the southern Weddell Sea. We propose that there are two reasons for the discrepancies in our model: the source waters are not as homogenous as the model assumes; and there are geographical and seasonal variations ofCO 2 exchange with the atmosphere and the input of inorganic carbon and nitrate from below the mixed layer resulting in imbalances in the mixed layer concentration ratios.en
dc.format.extent55009 byteseng
dc.format.extent2314258 byteseng
dc.format.extent166 byteseng
dc.format.mimetypetext/plaineng
dc.format.mimetypeapplication/pdfeng
dc.format.mimetypetext/plaineng
dc.language.isoengeng
dc.publisherElseviereng
dc.titleInterannual controls on Weddell Sea surface water fCO2 during the autumn–winter transition phaseeng
dc.typeJournal articleeng
dc.typePeer reviewedeng
dc.rights.holderCopyright 2004 Elsevier Ltd.
bora.peerreviewedPeer reviewedeng
bibo.doihttp://dx.doi.org/10.1016/j.dsr.2004.01.002eng
dc.identifier.doihttp://dx.doi.org/10.1016/j.dsr.2004.01.002


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