Identificador persistente para citar o vincular este elemento: http://hdl.handle.net/10553/74799
Campo DC Valoridioma
dc.contributor.advisorArístegui Ruiz, Javier-
dc.contributor.advisorSangrá Inciarte, Pablo-
dc.contributor.authorVelasco Senovilla, Esther-
dc.date.accessioned2020-10-16T11:40:30Z-
dc.date.available2020-10-16T11:40:30Z-
dc.date.issued2017en_US
dc.identifier.urihttp://hdl.handle.net/10553/74799-
dc.description.abstractMesoscale and submesoscale features of associated with the eddy field located downstream of the island of Gran Canaria are studied to assess their impact on the structure and distribution of the planktonic community. This study shows hydrographic and biological information based on XBT (Expendable Bathythermographs) and biogeochemical Rosette-CTD casts at a high resolution (near submesoscale) crossing a cyclonic eddy and its marginal frontal regions. Along the transect 4 main features were monitored: the margin of a large anticyclonic eddy, a large cyclonic eddy (affected by a filament from the North Africa Upwelling System), the sharp front between the two eddies, and a small submesoscale anticyclonic eddy. The “Vertical Oceanic Pump” (VOP) in the zone is typified by two main mechanisms, eddy-pumping, generated by the cyclonic eddy, and ASC (ageostrophic secondary circulation), produced at the fronts. Both processes affect the physicochemical nature of the water column, encompassing nutrient distribution. The planktonic community, which includes bacteria, cyanobacteria (Synechococcus and Prochlorococcus), autotrophic picoeukaryotes, and heterotrophic and autotrophic nanoflagellates show a heterogeneous distribution close to the submesoscale range. The analysis suggests that physical forcing (eddy pumping and ASC) is the main reason for the distribution of organisms, together with the filament, which introduces upwelled waters modifying the concentration of nutrients and organisms. The greatest accomplishment of this study compared with other eddy field studies, is that we have used a smaller scale resolution to look in detail and understand the physical forcing on the planktonic community distribution, and hence in the VOP associated with mesoscale features. Our results suggest that processes at submesoscale have a large effect on biogeochemical processes in the ocean, where eddies and frontal structures are dominant.en_US
dc.languageengen_US
dc.relationRemolinos Oceanicos y de Posición Atmosferica (Roda): Dinámica y Monitorización de Remolinos Oceanicos en la Corriente de Canariasen_US
dc.subject251001 Oceanografía biológicaen_US
dc.subject251007 Oceanografía físicaen_US
dc.subject.otherÁreas de afloramientoen_US
dc.subject.otherFitoplancton marinoen_US
dc.subject.otherTorbellinos (Mecánica de fluidos)en_US
dc.titleImpact of a cyclonic mesoscale eddy on the structure of the planktonic community at the submesoscale rangeen_US
dc.typeinfo:eu-repo/semantics/masterThesisen_US
dc.typeMasterThesisen_US
dc.contributor.departamentoDepartamento de Biologíaen_US
dc.contributor.facultadFacultad de Ciencias del Maren_US
dc.investigacionCienciasen_US
dc.type2Trabajo final de másteren_US
dc.description.notasMáster Universitario en Oceanografía ; 2016-2017en_US
dc.utils.revisionen_US
dc.identifier.matriculaTFT-41082es
dc.identifier.ulpgcen_US
dc.contributor.buulpgcBU-BASen_US
dc.contributor.titulacionMáster Universitario en Oceanografía por la Universidad de Cádiz, la Universidad de Las Palmas de Gran Canaria y la Universidad de Vigoes
item.grantfulltextopen-
item.fulltextCon texto completo-
crisitem.project.principalinvestigatorSangrá Inciarte, Pablo-
crisitem.advisor.deptGIR IOCAG: Oceanografía Biológica y Algología Aplicada-
crisitem.advisor.deptIU de Oceanografía y Cambio Global-
crisitem.advisor.deptDepartamento de Biología-
Colección:Trabajo final de máster
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