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Fortnightly changes in water transport direction across the mouth of a narrow estuary

dc.contributor.authorGarel, Erwan
dc.contributor.authorFerreira, Óscar
dc.date.accessioned2018-11-06T14:40:28Z
dc.date.available2018-11-06T14:40:28Z
dc.date.issued2013
dc.description.abstractThis research investigates the dynamics of the axial tidal flow and residual circulation at the lower Guadiana Estuary, south Portugal, a narrow mesotidal estuary with low freshwater inputs. Current data were collected near the deepest part of the channel for 21 months and across the channel during two (spring and neap) tidal cycles. Results indicate that at the deep channel, depth-averaged currents are stronger and longer during the ebb at spring and during the flood at neap, resulting in opposite water transport directions at a fortnightly time scale. The net water transport across the entire channel is up-estuary at spring and down-estuary at neap, i.e., opposite to the one at the deep channel. At spring tide, when the estuary is considered to be well mixed, the observed pattern of circulation (outflow in the deep channel, inflow over the shoals) results from the combination of the Stokes transport and compensating return flow, which varies laterally with the bathymetry. At neap tide (in particular for those of lowest amplitude each month), inflows at the deep channel are consistently associated with the development of gravitational circulation. Comparisons with previous studies suggest that the baroclinic pressure gradient (rather than internal tidal asymmetries) is the main driver of the residual water transport. Our observations also indicate that the flushing out of the water accumulated up-estuary (at spring) may also produce strong unidirectional barotropic outflow across the entire channel around neap tide.pt_PT
dc.description.sponsorshipReeq/484/MAR/2005; SFRH/BPD/34475/2005
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.doi10.1007/s12237-012-9566-zpt_PT
dc.identifier.issn1559-2723
dc.identifier.otherAUT: OFE00989;
dc.identifier.urihttp://hdl.handle.net/10400.1/10903
dc.language.isoengpt_PT
dc.peerreviewedyespt_PT
dc.subjectMass transport velocitypt_PT
dc.subjectStokes transportpt_PT
dc.subjectEstuarine circulationpt_PT
dc.subjectSpring–neap variabilitypt_PT
dc.titleFortnightly changes in water transport direction across the mouth of a narrow estuarypt_PT
dc.typejournal article
dspace.entity.typePublication
oaire.citation.endPage299pt_PT
oaire.citation.issue2pt_PT
oaire.citation.startPage286pt_PT
oaire.citation.titleEstuaries and Coastspt_PT
oaire.citation.volume36pt_PT
person.familyNameGarel
person.familyNameFerreira
person.givenNameErwan
person.givenNameÓscar
person.identifier.ciencia-id5D13-7EA7-6C6D
person.identifier.ciencia-id1F1C-DF44-94C9
person.identifier.orcid0000-0002-4584-9759
person.identifier.orcid0000-0001-9975-0036
person.identifier.ridN-9811-2014
person.identifier.scopus-author-id23491739700
rcaap.rightsopenAccesspt_PT
rcaap.typearticlept_PT
relation.isAuthorOfPublication7e619cba-3bfb-4964-bdf3-b8afd91a4a29
relation.isAuthorOfPublication14adf536-4f81-42de-b00f-6d1cf3b0d75e
relation.isAuthorOfPublication.latestForDiscovery7e619cba-3bfb-4964-bdf3-b8afd91a4a29

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