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Fortnightly switching of residual flow drivers produced by seawater intrusion in a long, non-rotating estuary

dc.contributor.authorGarel, Erwan
dc.contributor.authorKhosravi, Maziar
dc.contributor.authorValle-Levinson, Arnoldo
dc.contributor.authorDíez-Minguito, Manuel
dc.date.accessioned2025-10-13T12:34:04Z
dc.date.available2025-10-13T12:34:04Z
dc.date.issued2025-09-20
dc.description.abstractTowed and moored ADCP and salinity measurements were collected in Summer 2023 at two cross-channel transects of the 80-km-long Guadiana Estuary, at 4 km and 20 km from the mouth, during low (< 10 m(3)/s) river discharge conditions. The dataset indicates that the lateral structure of axial residual flows changed from vertically sheared to laterally sheared with tidal forcing. These structures resemble theoretical expectations for a density-driven or eddy viscosity-shear covariance (ESCO) circulation at neap tide and for a tidally driven circulation produced by longitudinal advection (tidal stress) at spring tide. The tidal variability of the residual flow magnitude and of the contributions of unidirectional or two-layer vertical profiles indicate that the primary driver of the residual circulation changes between neap tide and spring tide. Seawater (i.e. with salinity > 35 kg/g) intrusion was several kilometres, equivalent to similar to 1/8 of the estuary's length. As a result, the horizontal density gradient was weakest near the mouth where the residual circulation was barotropic, produced by tidal stress at spring tide and possibly by an ESCO mechanism at neap tide. At 20 km upstream, the dominant driver switched from tidal stress at spring tide to a baroclinic (and potentially ESCO) circulation at neap tide. At this location, scaling analyses of the tidally averaged momentum equation using the densimetric tidal Froude number supported the idea of dominance of tidal stress at spring tide.eng
dc.identifier.doi10.1007/s12237-025-01605-1
dc.identifier.eissn1559-2731
dc.identifier.issn1559-2723
dc.identifier.urihttp://hdl.handle.net/10400.1/27821
dc.language.isoeng
dc.peerreviewedyes
dc.publisherSpringer
dc.relationCentre for Marine and Environmental Research (CIMA)
dc.relationAquatic Research Infrastructure Network
dc.relation.ispartofEstuaries and Coasts
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/
dc.subjectADCP
dc.subjectBaroclinic
dc.subjectBarotropic
dc.subjectTidal froude number
dc.subjectLow river discharge
dc.titleFortnightly switching of residual flow drivers produced by seawater intrusion in a long, non-rotating estuaryeng
dc.typejournal article
dspace.entity.typePublication
oaire.awardTitleCentre for Marine and Environmental Research (CIMA)
oaire.awardTitleAquatic Research Infrastructure Network
oaire.awardURIinfo:eu-repo/grantAgreement/FCT/6817 - DCRRNI ID/UIDP%2F00350%2F2020/PT
oaire.awardURIinfo:eu-repo/grantAgreement/FCT/6817 - DCRRNI ID/LA%2FP%2F0069%2F2020/PT
oaire.citation.issue6
oaire.citation.startPage176
oaire.citation.titleEstuaries and Coasts
oaire.citation.volume48
oaire.fundingStream6817 - DCRRNI ID
oaire.fundingStream6817 - DCRRNI ID
oaire.versionhttp://purl.org/coar/version/c_970fb48d4fbd8a85
person.familyNameGarel
person.familyNameKhosravi
person.givenNameErwan
person.givenNameMaziar
person.identifier.ciencia-id5D13-7EA7-6C6D
person.identifier.orcid0000-0002-4584-9759
person.identifier.orcid0000-0002-4189-6312
person.identifier.ridN-9811-2014
person.identifier.scopus-author-id23491739700
project.funder.identifierhttp://doi.org/10.13039/501100001871
project.funder.identifierhttp://doi.org/10.13039/501100001871
project.funder.nameFundação para a Ciência e a Tecnologia
project.funder.nameFundação para a Ciência e a Tecnologia
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relation.isAuthorOfPublication2aa5e74a-8a70-4f11-a079-4784183bc982
relation.isAuthorOfPublication.latestForDiscovery7e619cba-3bfb-4964-bdf3-b8afd91a4a29
relation.isProjectOfPublication62b4d568-8b21-464c-97ed-de826eab4136
relation.isProjectOfPublication5af011f9-3888-449a-a18c-d08b59e87091
relation.isProjectOfPublication.latestForDiscovery62b4d568-8b21-464c-97ed-de826eab4136

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