Please use this identifier to cite or link to this item: http://hdl.handle.net/10553/122124
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dc.contributor.authorAldrich Rodríguez, Ariadnaen_US
dc.contributor.authorGonzález Dávila, Melchoren_US
dc.contributor.authorSantana Casiano, Magdalenaen_US
dc.contributor.authorGonzález González, Aridaneen_US
dc.date.accessioned2023-04-27T09:45:12Z-
dc.date.available2023-04-27T09:45:12Z-
dc.date.issued2023en_US
dc.identifier.isbn978-84-9042-477-3en_US
dc.identifier.urihttp://hdl.handle.net/10553/122124-
dc.description.abstractThis study describes the annual pattern, from March 2020 to April 2021, of different parameters of the CO2 system and ocean acidification in the eastern coast of Gran Canaria Island (Gando Bay) via the monitoring of pHT, total dissolved inorganic carbon (CT), total alkalinity (AT) and CO2 fugacity (fCO2), as well as other parameters such as sea surface salinity and temperature (SSS and SST), dissolved oxygen (O2), chlorophyll (chl-a) and wind. In addition, the flux of CO2 (FCO2) between the atmosphere and the sea surface has been computed. The results show a clear seasonal fCO2 variation in seawater from 380 μatm (in winter) to 430 μatm (in summer), where the opposite behaviour was observed in pHT with a range of variation of 8.072 to 8.032 and CT between 2123.2 and 2101.5 μmol kg-1. The thermal/nonthermal processes (ratio T/NT) affect the seasonal fCO2 in seawater with a value of 1.38. The temperature mainly controls the variability of fCO2 in the region, but the non-thermal factors have a higher contribution than other studies in the open ocean. Results indicate a higher role of the primary production in the area, which reduces CT and the fCO2. In addition, the rise of a water mass with low salinity (36.4) and temperature (22 ºC) due to the effect of high and constant Trade Winds (July and August), contribute to the physical and chemical seasonal variability in the Bay. This water mass had also higher concentrations of CT due to the remineralization of organic matter that takes place at depth and out of the Bay. The calculated flux of CO2 at the buoy location was 0.27 ± 0.22 mmol m-2 d-1, showing a mean behaviour as a slight source of CO2. Assuming this value for all Gando Bay, it was found that the area emits 4.58 ± 3.68 Tons yr-1 of CO2 each year. This coastal time-series in the Canary Islands is contributing to improve our knowledge about the impacts of climate change in the CO2 system and ocean acidification in coastal systems, also, incrementing the data set for the global carbon budget.en_US
dc.languageengen_US
dc.publisherServicio de Publicaciones y Difusión Científica de la Universidad de Las Palmas de Gran Canaria (ULPGC)en_US
dc.relationConvenio Específico de Cooperación Entre la Universidad de Las Palmas de Gran Canaria y la Consejería de Transición Ecológica, lucha contra el cambio climático y planificación territorial del Gobierno de Canarias para el mantenimiento de la red de Observación de Dióxido de Carbono Oceánico en Canarias (CARBOCAN)en_US
dc.sourceAbstracts Volume VIII International Symposium on Marine Sciences, July 2022 / coordinación, María Esther Torres Padrón, p. 360-361en_US
dc.subject251002 Oceanografía químicaen_US
dc.subject.otherCO2 systemen_US
dc.subject.otherCO2 fluxesen_US
dc.subject.otherCoastal acidificationen_US
dc.subject.otherCoastal time-seriesen_US
dc.titleSeasonal variability of CO2 system and air-sea fluxes on the east coast of Gran Canariaen_US
dc.typeinfo:eu-repo/semantics/conferenceObjecten_US
dc.typeConference posteren_US
dc.relation.conferenceVIII International Symposium on Marine Sciences (ISMS 2022)en_US
dc.description.lastpage361en_US
dc.description.firstpage360en_US
dc.investigacionCienciasen_US
dc.type2Póster de congresosen_US
dc.description.numberofpages2en_US
dc.utils.revisionen_US
dc.identifier.ulpgcen_US
dc.contributor.buulpgcBU-BASen_US
dc.contributor.buulpgcBU-BASen_US
dc.contributor.buulpgcBU-BASen_US
dc.contributor.buulpgcBU-BASen_US
item.grantfulltextopen-
item.fulltextCon texto completo-
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.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.orcid0000-0002-5637-8841-
crisitem.author.parentorgIU de Oceanografía y Cambio Global-
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.author.fullNameGonzález González, Aridane-
crisitem.project.principalinvestigatorGonzález Dávila, Melchor-
crisitem.event.eventsstartdate06-07-2022-
crisitem.event.eventsenddate08-07-2022-
Appears in Collections:Póster de congreso
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