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dc.contributor.authorLaiz, Irene
dc.contributor.authorFerrer, Luis
dc.contributor.authorPlomaritis, Theocharis A.
dc.contributor.authorCharria, Guillaume
dc.date.accessioned2017-10-23T11:15:28Z-
dc.date.available2017-10-23T11:15:28Z-
dc.date.issued2014
dc.identifierISI:000343345300005
dc.identifier.citationDEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 2014, 106, 49-67
dc.identifier.issn0967-0645
dc.identifier.urihttp://dspace.azti.es/handle/24689/334-
dc.description.abstractDaily time series of in-situ tide gauge records and river runoff data were analysed to investigate the contribution of river discharge storm events to sea level in the Bay of Biscay. Three main river systems were considered for this study, representing cases of small (Nervion, 1900 km(2)), medium (Adour, 16,880 km(2)) and large (Gironde, 84,811 km(2)) watershed basins. Typical storms correspond to water discharge rates of 150, 700, and 1100 m(3) s(-1) from the Nervion, Adour, and Gironde rivers, respectively. The effect of these events on daily mean sea level was evaluated using two different approaches: (1) through the analysis of time series of tide gauges placed within the river mouths; and (2) through numerical simulations using the ROMS model (Regional Ocean Modeling System). The three selected tide gauges are located at Bilbao (Spain) for the Nervion river, Boucau-Bayonne (France) for the Adour river and Port-Bloc (France) for the Gironde river. River runoff extreme events were more notable at the two tide gauges located within the largest rivers, namely, Adour and Gironde, where approximately 13\% and 53.6\% of the pressure-adjusted sea-level variance was explained by those events. The results obtained from the ROMS simulations suggest that the main effect of river discharge storm events occurs as a response to the input of lower salinity water. This plume of overlaying less dense water would produce a sea-level increase around the river mouth and along the coast, suggesting the generation of a coastal density current through the balance between the Coriolis force and the cross-shore pressure gradient. The main area of influence of the selected river discharges was confined to the river mouth for the Nervion, but extended up to approximately 28 km (33 km) offshore for the Adour (Gironde) river, before turning northward to flow as a density current along the coast. (C) 2014 Elsevier Ltd. All rights reserved.
dc.description.sponsorshipDr. Laiz was supported by the Ministerio de Ciencia e Innovacion (Spain) through Project ``CLI-CGL2008-04736��. Dr. Plomaritis was supported by the EU FP7 Environment Research Programme through Project ``MICORE�� (Project number 202798). We thank the tide gauge observation reference networks.(French designation REFMAR) and the SONEL data assembly centre for providing tide gauge data at Port-Bloc and Boucau-Bayonne as well as Puertos del Estado (Spain) for providing the Bilbao tide gauge data. The Diputacion Foral de Bizcaia (Spain) and the Banque Nationale d'Hydrometrie et d'Hydrologie (France) are also acknowledged for making available the river discharge rates.
dc.language.isoeng
dc.publisherPERGAMON-ELSEVIER SCIENCE LTD
dc.subjectBay of Biscay
dc.subjectSea level
dc.subjectTide gauges
dc.subjectRiver discharge
dc.subjectROMS modelling
dc.subjectFRENCH CONTINENTAL-SHELF
dc.subjectNORTH-ATLANTIC
dc.subjectSOUTHERN BAY
dc.subjectWAVELET ANALYSIS
dc.subjectCURRENT SYSTEM
dc.subjectCENTRAL WATER
dc.subjectCELTIC SEA
dc.subjectSURFACE
dc.subjectEDDIES
dc.subjectCIRCULATION
dc.titleEffect of river runoff on sea level from in-situ measurements and numerical models in the Bay of Biscay
dc.typeArticle
dc.identifier.journalDEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY
dc.format.page49-67
dc.format.volume106
dc.contributor.funderMinisterio de Ciencia e Innovacion (Spain) [CLI-CGL2008-04736]
dc.contributor.funderEU FP7 Environment Research Programme through Project ``MICORE�� [202798]
dc.identifier.e-issn1879-0100
dc.identifier.doi10.1016/j.dsr2.2013.12.013
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