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dc.contributor.advisorDíez Minguito, Manuel es_ES
dc.contributor.authorSerrano García, María Ángeleses_ES
dc.contributor.otherUniversidad de Granada. Departamento de Estructuras e Ingeniería Hidráulicaes_ES
dc.date.accessioned2017-01-31T12:44:01Z
dc.date.available2017-01-31T12:44:01Z
dc.date.issued2016
dc.date.submitted2016-12-16
dc.identifier.citationSerrano García, M.A. Alborán sea shelf hydrodynamic processes. Granada: Universidad de Granada, 2016. [http://hdl.handle.net/10481/44573]es_ES
dc.identifier.isbn9788491630654
dc.identifier.urihttp://hdl.handle.net/10481/44573
dc.description.abstractThe Alborán Sea is a back-arc region located in the western Mediterranean Sea. This region is connected to the Atlantic Ocean through the Gibraltar Strait and opens to the east into the Balearic Basin through the Alborán Trough. In the Alborán Sea, oceanic motions involve a great variety of both spatial and temporal scales. The influence of tides, subinertial flow induced by atmospheric pressure gradients and wind stress, and the wind waves near the coast has been intensively studied. However, a detailed study of long-period waves, as Continental Shelf Waves (CSWs), propagating along the continental shelves of the Alborán Sea is still lacking. This type of waves propagates in one direction with the coast on the right (Northern Hemisphere). The presence of two narrow, opposite, and approximately parallel continental shelves provides an additional interest to the study site, because of the possible interaction of these kind of waves travelling in opposite directions. Then, this Thesis studies the existence of these waves in the continental shelves of the Alborán Sea. Another special feature of the Alborán Sea is that it is indented by transverse incisions. Some of these incisions are large enough to be considered submarine canyons. Several studies suggest that wind modifies the circulation in submarine canyons and drives cross-shore transports and vertical motions. However, little is known on the role of local atmospheric pressure gradients on the circulation of a submarine canyon. This Thesis also explores the role of this forcing in the circulation of a submarine canyon of the Alborán Sea, the Jolúcar canyon. Thus, the general aim of this Thesis is to study hydrodynamic processes over the continental shelves (northern and southern) of Alborán Sea (regional scale) and the local circulation in a submarine canyon indenting in the northern shelf. The objective is addressed using data analysis of field observations, and semi-analytical models.en_EN
dc.description.sponsorshipTesis Univ. Granada. Programa Oficial de Doctorado en: Dinámica de Flujos Biogeoquímicos y sus aplicacioneses_ES
dc.format.mimetypeapplication/pdfen_US
dc.language.isoenges_ES
dc.publisherUniversidad de Granadaes_ES
dc.rightsCreative Commons Attribution-NonCommercial-NoDerivs 3.0 Licenseen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/en_US
dc.subjectAlboránes_ES
dc.subjectHidrodinámica es_ES
dc.subjectOndas es_ES
dc.subjectPlataforma continental es_ES
dc.subjectCinemática es_ES
dc.titleAlborán sea shelf hydrodynamic processesen_EN
dc.typeinfo:eu-repo/semantics/doctoralThesises_ES
dc.subject.udc551.46es_ES
dc.subject.udc556.3es_ES
dc.subject.udc220504es_ES
europeana.typeTEXTen_US
europeana.dataProviderUniversidad de Granada. España.es_ES
europeana.rightshttp://creativecommons.org/licenses/by-nc-nd/3.0/en_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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