Please use this identifier to cite or link to this item: http://hdl.handle.net/10553/6216
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dc.contributor.authorGonzález-Dávila, M.en_US
dc.contributor.authorSantana-Casiano, J. M.en_US
dc.contributor.authorFine, R. A.en_US
dc.contributor.authorHappell, Jimen_US
dc.contributor.authorDelille, B.en_US
dc.contributor.authorSpeich, S.en_US
dc.contributor.otherSpeich, Sabrina-
dc.contributor.otherSANTANA CASIANO, JUANA MAGDALENA-
dc.contributor.otherDelille, Bruno-
dc.contributor.otherGONZALEZ DAVILA, MELCHOR-
dc.date.accessioned2011-08-09T02:31:00Z
dc.date.accessioned2018-03-08T13:08:27Z-
dc.date.available2011-08-09T09:28:18Z
dc.date.available2018-03-08T13:08:27Z-
dc.date.issued2011en_US
dc.identifier.issn1726-4170en_US
dc.identifier.urihttp://hdl.handle.net/10553/6216-
dc.description.abstractCarbonate system variables were measured in the South Atlantic sector of the Southern Ocean along a transect from South Africa to the southern limit of the Antarctic Circumpolar Current (ACC) from February to March 2008. Eddies detached from the retroflection of the Agulhas Current increased the gradients observed along the fronts. Minima in the fugacity of CO2, fCO2, and maxima in pH on either side of the frontal zone were observed, noting that within the frontal zone fCO2 reached maximum values and pH was at a minimum. Vertical distributions of water masses were described by their carbonate system properties and their relationship to CFC concentrations. Upper Circumpolar Deep Water (UCDW) and Lower Circumpolar Deep Water (LCDW) offered pHT,25 values of 7.56 and 7.61, respectively. The UCDW also had higher concentrations of CFC-12 (>0.2 pmol kg−1) as compared to deeper waters, revealing that UCDW was mixed with recently ventilated waters. Calcite and aragonite saturation states (Ω) were also affected by the presence of these two water masses with high carbonate concentrations. The aragonite saturation horizon was observed at 1000 m in the subtropical area and north of the Subantarctic Front. At the position of the Polar Front, and under the influence of UCDW and LCDW, the aragonite saturation horizon deepened from 800 m to 1500 m at 50.37° S, and reached 700 m south of 57.5° S. High latitudes proved to be the most sensitive areas to predicted anthropogenic carbon increase. Buffer coefficients related to changes in [CO2], [H+] and Ω with changes in dissolved inorganic carbon (CT) and total alkalinity (AT) offered minima values in the Antarctic Intermediate Water and UCDW layers. These coefficients suggest that a small increase in CT will sharply decrease the status of pH and carbonate saturation. Here we present data that suggest that south of 55° S, surface water will be under-saturated with respect to aragonite within the next few decades.en_US
dc.formatapplication/pdfes
dc.languageengen_US
dc.relationBiogeoquimica Del Oceano Sur: Bonus Goodhopeen_US
dc.relation.ispartofBiogeosciencesen_US
dc.rightsby-nc-ndes
dc.sourceBiogeosciences [ISSN 1726-4170], v. 8 (5), p. 1401-1413en_US
dc.subject.otherAntarctic Circumpolar Currenten_US
dc.subject.otherWeddell Gyreen_US
dc.subject.otherInterannual Variabilityen_US
dc.subject.otherAtmospheric Co2en_US
dc.subject.otherCanary-Islandsen_US
dc.subject.otherClimate-Changeen_US
dc.subject.otherIndian Sectoren_US
dc.subject.otherSeawateren_US
dc.subject.otherDioxideen_US
dc.subject.otherAfricaen_US
dc.titleCarbonate system in the water masses of the Southeast Atlantic sector of the Southern Ocean during February and March 2008en_US
dc.typeinfo:eu-repo/semantics/Articleen_US
dc.typeArticleen_US
dc.identifier.doi10.5194/bg-8-1401-2011en_US
dc.identifier.scopus79958034640-
dc.identifier.isi000291942000002-
dcterms.isPartOfBiogeosciences
dcterms.sourceBiogeosciences[ISSN 1726-4170],v. 8 (5), p. 1401-1413
dc.contributor.authorscopusid6603931257-
dc.contributor.authorscopusid6701344294-
dc.contributor.authorscopusid7201538303-
dc.contributor.authorscopusid6602193023-
dc.contributor.authorscopusid6602185381-
dc.contributor.authorscopusid6602115663-
dc.identifier.absysnet630984-
dc.identifier.crisid2199;1562;-;-;-;-
dc.description.lastpage1413en_US
dc.description.firstpage1401en_US
dc.relation.volume8en_US
dc.investigacionCienciasen_US
dc.rights.accessrightsinfo:eu-repo/semantics/openAccesses
dc.rights.accessrightsinfo:eu-repo/semantics/openAccesses
dc.type2Artículoen_US
dc.identifier.wosWOS:000291942000002-
dc.contributor.daisngid518149-
dc.contributor.daisngid579253-
dc.contributor.daisngid465296-
dc.contributor.daisngid1931953-
dc.contributor.daisngid484917-
dc.contributor.daisngid616508-
dc.identifier.investigatorRIDL-3780-2014-
dc.identifier.investigatorRIDK-5058-2014-
dc.identifier.investigatorRIDC-3486-2008-
dc.identifier.investigatorRIDK-4958-2014-
dc.utils.revisionen_US
dc.contributor.wosstandardWOS:Gonzalez-Davila, M-
dc.contributor.wosstandardWOS:Santana-Casiano, JM-
dc.contributor.wosstandardWOS:Fine, RA-
dc.contributor.wosstandardWOS:Happell, J-
dc.contributor.wosstandardWOS:Delille, B-
dc.contributor.wosstandardWOS:Speich, S-
dc.date.coverdateJunio 2011en_US
dc.identifier.supplement2199;1562;-;-;-;--
dc.identifier.supplement2199;1562;-;-;-;--
dc.identifier.supplement2199;1562;-;-;-;--
dc.identifier.ulpgcen_US
dc.contributor.buulpgcBU-BASen_US
dc.description.sjr2,524
dc.description.jcr3,859
dc.description.sjrqQ1
dc.description.jcrqQ1
dc.description.scieSCIE
item.fulltextCon texto completo-
item.grantfulltextopen-
crisitem.author.deptGIR IOCAG: Química Marina-
crisitem.author.deptIU de Oceanografía y Cambio Global-
crisitem.author.deptDepartamento de Química-
crisitem.author.deptGIR IOCAG: Química Marina-
crisitem.author.deptIU de Oceanografía y Cambio Global-
crisitem.author.deptDepartamento de Química-
crisitem.author.orcid0000-0003-3230-8985-
crisitem.author.orcid0000-0002-7930-7683-
crisitem.author.parentorgIU de Oceanografía y Cambio Global-
crisitem.author.parentorgIU de Oceanografía y Cambio Global-
crisitem.author.fullNameGonzález Dávila, Melchor-
crisitem.author.fullNameSantana Casiano, Juana Magdalena-
crisitem.project.principalinvestigatorGonzález Dávila, Melchor-
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