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Spatiotemporal variability of the coastal circulation in the northern Gulf of Cadiz from Copernicus Sentinel-3A satellite radar altimetry measurements

datacite.subject.sdg14:Proteger a Vida Marinha
datacite.subject.sdg13:Ação Climática
datacite.subject.sdg09:Indústria, Inovação e Infraestruturas
dc.contributor.authorMulero-Martinez, R.
dc.contributor.authorGómez-Enri, J.
dc.contributor.authorde Oliveira Júnior, Luciano
dc.contributor.authorGarel, Erwan
dc.contributor.authorRelvas, Paulo
dc.contributor.authorMañanes, R.
dc.date.accessioned2026-04-13T13:33:05Z
dc.date.available2026-04-13T13:33:05Z
dc.date.issued2024-05
dc.description.abstractThis study presents a generalised characterisation of the surface circulation over the northern shelf of the Gulf of Cadiz, based on 4 years of high-resolution satellite altimetry data from Sentinel-3A and wind model data. The altimetry-based surface zonal currents, adjusted for bottom-drag and wind effects, are compared with a generic CMEMS product and validated against in-situ ADCP measurements. The proposed altimetry product demonstrates superior performance than the CMEMS product, accurately reflecting surface circulation direction compared to in-situ measurements (r = 0.77, RMSE = 0.10 m/s, bias = 0.01 m/s). The use of the bottom-drag and wind-corrected/uncorrected altimetry product for spatiotemporal analysis of the shelf circulation revealed the distinct contributions of wind-driven and geostrophic components in different basin sectors. The results show that over the western basin, positive (eastward) sur face currents were predominantly driven by westerly winds, while only occasionally, westward flows coincided with easterly winds, suggesting a higher control of the geostrophic component over the westward flows. In contrast, over the eastern basin, both eastward and westward flows were found to be primarily driven by favourable winds. Additionally, the analysis of Absolute Dynamic Topography (ADT) values along the whole basin showed the presence of ADT gradients both along-shore and cross-shore over the shelf, contributing to geostrophic flows. Finally, the seasonal analysis showed that eastward circulation tends to dominate during the spring and summer months, related to the upwelling season in the Gulf of Cadiz and associated westerly winds. Westward flows prevail during the winter months, related to easterly winds and the rebalancing of the along-shore sea level gradient during relaxed upwelling conditions. The findings demonstrate a significant improvement in the use of satellite altimetry data to study complex oceanographic dynamics in coastal areas, where both spatial and temporal variability are high. Moreover, the similarity of our results to those obtained from in-situ systems supports the use of altimetry data and publicly available wind models to support oceanographic studies in remote or resource-limited areas.eng
dc.identifier.doi10.1016/j.asr.2024.02.054
dc.identifier.issn0273-1177
dc.identifier.urihttp://hdl.handle.net/10400.1/28659
dc.language.isoeng
dc.peerreviewedyes
dc.publisherElsevier
dc.relation.ispartofAdvances in Space Research
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/
dc.subjectCoastal altimetry
dc.subjectCoastal oceanography
dc.subjectSentinel-3
dc.subjectGulf of Cadiz
dc.subjectSurface circulation
dc.subjectWind speed
dc.titleSpatiotemporal variability of the coastal circulation in the northern Gulf of Cadiz from Copernicus Sentinel-3A satellite radar altimetry measurementseng
dc.typejournal article
dspace.entity.typePublication
oaire.citation.endPage4936
oaire.citation.issue10
oaire.citation.startPage4922
oaire.citation.titleAdvances in Space Research
oaire.citation.volume73
oaire.versionhttp://purl.org/coar/version/c_970fb48d4fbd8a85
person.familyNamede Oliveira Júnior
person.familyNameGarel
person.familyNameRelvas
person.givenNameLuciano
person.givenNameErwan
person.givenNamePaulo
person.identifier.ciencia-idEA1D-0D5C-8C56
person.identifier.ciencia-id5D13-7EA7-6C6D
person.identifier.ciencia-id2412-1F65-A044
person.identifier.orcid0000-0001-5899-2979
person.identifier.orcid0000-0002-4584-9759
person.identifier.orcid0000-0002-6404-5895
person.identifier.ridN-9811-2014
person.identifier.ridB-1257-2008
person.identifier.scopus-author-id23491739700
person.identifier.scopus-author-id6505976206
relation.isAuthorOfPublicationbdfdf659-6b7b-4ef9-ac90-2781469b8946
relation.isAuthorOfPublication7e619cba-3bfb-4964-bdf3-b8afd91a4a29
relation.isAuthorOfPublication94f4d10b-242d-4560-b716-6375f1a01eac
relation.isAuthorOfPublication.latestForDiscovery7e619cba-3bfb-4964-bdf3-b8afd91a4a29

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