Please use this identifier to cite or link to this item: http://hdl.handle.net/10553/49801
DC FieldValueLanguage
dc.contributor.authorde la Paz, Mercedesen_US
dc.contributor.authorHuertas, Emma M.en_US
dc.contributor.authorPadín, Xose Antonioen_US
dc.contributor.authorGónzalez-Dávila, Melchoren_US
dc.contributor.authorSantana-Casiano, Magdalenaen_US
dc.contributor.authorForja, Jesús M.en_US
dc.contributor.authorOrbi, Abdellatifen_US
dc.contributor.authorPérez, Fiz F.en_US
dc.contributor.authorRíos, Aida F.en_US
dc.contributor.otherFernandez Perez, Fiz-
dc.contributor.otherGONZALEZ DAVILA, MELCHOR-
dc.contributor.otherSANTANA CASIANO, JUANA MAGDALENA-
dc.contributor.otherHUERTAS, EMMA-
dc.contributor.otherORBI, ABDELLATIF-
dc.contributor.otherde la Paz, Mercedes-
dc.contributor.otherForja Pajares, Jesus-
dc.date.accessioned2018-11-24T10:50:22Z-
dc.date.available2018-11-24T10:50:22Z-
dc.date.issued2011en_US
dc.identifier.issn0304-4203en_US
dc.identifier.urihttp://hdl.handle.net/10553/49801-
dc.description.abstractThe present study reports and discusses water surface fCO2 measurements from 36 cruises in the Strait of Gibraltar made over an eleven-year period (1997 to 2009). Underway measurements of sea surface CO2 fugacity (fCO2sw), sea surface temperature (SST) and sea surface salinity (SSS) compiled during the cruises were analysed and integrated into a single database which provided the resolution/sensitivity required for an examination of the seasonal variability of the fCO2sw; these data allowed the reconstruction of the climatological seasonal cycle for the year 2005. The seasonal cycle of both SST and SSS was found to be within the range of the thermohaline signature of the North Atlantic Surface Water, which is the main water mass that flows into the Mediterranean Sea through the Strait of Gibraltar at the surface. The seasonal distribution of fCO22005 was characterised by a monthly minimum value of 334 ± 12 μatm in May, followed by a gradual increase to a maximum of 385 μatm during late summer, due to the warming of surface waters. The spatial variability of fCO2sw observed in the area also indicated that superimposed phenomena, occurring at scales other than seasonal, could affect the dissolved CO2 distribution. In particular, intense vertical mixing processes generated by internal waves in this region may have an impact on the surface fCO2sw on a tidal scale. Seasonal CO2 cycle dynamics indicated that the surface waters of the Strait of Gibraltar acted as an atmospheric CO2 source during summer and autumn and a CO2 sink during winter and spring. When these sink/source strengths are integrated on an annual basis, the Strait of Gibraltar was close to equilibrium with atmospheric CO2, resulting in a neutral atmosphere-ocean exchange (− 0.06 ± 0.12 mol C m− 2 yr− 1).en_US
dc.languageengen_US
dc.relationMarine Carbon Sources And Sinks Assessment (Carboocean)en_US
dc.relation.ispartofMarine Chemistryen_US
dc.sourceMarine Chemistry [ISSN 0304-4203], v. 126 (1-4), p. 155-162en_US
dc.subject251002 Oceanografía químicaen_US
dc.subject.otherCarbon dioxideen_US
dc.subject.otherAir–sea CO2 exchangeen_US
dc.subject.otherStrait of Gibraltaren_US
dc.subject.otherSeasonal variabilityen_US
dc.titleReconstruction of the seasonal cycle of air-sea CO2 fluxes in the Strait of Gibraltaren_US
dc.typeinfo:eu-repo/semantics/Articleen_US
dc.typeArticleen_US
dc.identifier.doi10.1016/j.marchem.2011.05.004
dc.identifier.scopus80051938054-
dc.identifier.isi000295195300016-
dcterms.isPartOfMarine Chemistry-
dcterms.sourceMarine Chemistry[ISSN 0304-4203],v. 126 (1-4), p. 155-162-
dc.contributor.authorscopusid22834170900-
dc.contributor.authorscopusid56313933300-
dc.contributor.authorscopusid16301932800-
dc.contributor.authorscopusid6603931257-
dc.contributor.authorscopusid6701344294-
dc.contributor.authorscopusid7003332206-
dc.contributor.authorscopusid55409027900-
dc.contributor.authorscopusid56598611300-
dc.contributor.authorscopusid7103240290-
dc.description.lastpage162en_US
dc.identifier.issue1-4-
dc.description.firstpage155en_US
dc.relation.volume126en_US
dc.investigacionCienciasen_US
dc.type2Artículoen_US
dc.contributor.daisngid3147146-
dc.contributor.daisngid1136370-
dc.contributor.daisngid1587730-
dc.contributor.daisngid518149-
dc.contributor.daisngid28303796
dc.contributor.daisngid579253-
dc.contributor.daisngid411610-
dc.contributor.daisngid2309784-
dc.contributor.daisngid145213-
dc.contributor.daisngid329342-
dc.identifier.investigatorRIDB-9001-2011-
dc.identifier.investigatorRIDK-4958-2014-
dc.identifier.investigatorRIDK-5058-2014-
dc.identifier.investigatorRIDA-9739-2010-
dc.identifier.investigatorRIDNo ID-
dc.identifier.investigatorRIDNo ID-
dc.identifier.investigatorRIDNo ID-
dc.utils.revisionen_US
dc.contributor.wosstandardWOS:de la Paz, M
dc.contributor.wosstandardWOS:Huertas, EM
dc.contributor.wosstandardWOS:Padin, XA
dc.contributor.wosstandardWOS:Gonzalez-Davila, M
dc.contributor.wosstandardWOS:Santana-Casiano, M
dc.contributor.wosstandardWOS:Forja, JM
dc.contributor.wosstandardWOS:Orbi, A
dc.contributor.wosstandardWOS:Perez, FF
dc.contributor.wosstandardWOS:Rios, AF
dc.date.coverdateSeptiembre 2011
dc.identifier.ulpgces
dc.description.sjr2,126
dc.description.jcr3,074
dc.description.sjrqQ1
dc.description.jcrqQ1
dc.description.scieSCIE
item.grantfulltextnone-
item.fulltextSin texto completo-
crisitem.project.principalinvestigatorGonzález Dávila, Melchor-
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.orcid0000-0002-7930-7683-
crisitem.author.orcid0000-0002-7930-7683-
crisitem.author.parentorgIU de Oceanografía y Cambio Global-
crisitem.author.parentorgIU de Oceanografía y Cambio Global-
crisitem.author.fullNameSantana Casiano, Juana Magdalena-
crisitem.author.fullNameSantana Casiano, Juana Magdalena-
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