Please use this identifier to cite or link to this item: http://hdl.handle.net/10773/24717
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dc.contributor.authorPicado, Anapt_PT
dc.contributor.authorLopes, Carina L.pt_PT
dc.contributor.authorMendes, Renatopt_PT
dc.contributor.authorVaz, Nunopt_PT
dc.contributor.authorDias, João M.pt_PT
dc.date.accessioned2018-11-27T14:19:57Z-
dc.date.available2018-11-27T14:19:57Z-
dc.date.issued2013-
dc.identifier.issn0749-0208pt_PT
dc.identifier.urihttp://hdl.handle.net/10773/24717-
dc.description.abstractStorm surges are a hazardous phenomenon, since they may flood large coastal areas, causing socio-economical and habitation losses. Thus, the study of their characteristics and effects in coastal regions is crucial to prevent their negative consequences. This work aims at assessing the storm surges impact in the hydrodynamics of a tidal lagoon located in the north-western Portuguese coast (Ria de Aveiro). Storm surge amplitudes of 0.58 m, 0.84 m and 1.17 m for 2, 10 and 100 return periods, respectively, were determined adjusting the annual maximum amplitudes to a Generalized Extreme Value (GEV) distribution. To assess the hydrodynamic changes in the Ria de Aveiro under storm surge conditions, numerical modeling simulations were carried out, considering four scenarios: a single astronomical tidal forcing (reference) and astronomical tide plus 2, 10 and 100 years return period surges. Maximum levels and velocities for the entire lagoon and the tidal prism for the main cross-sections were determined and compared with the reference scenario. Generally, the model results suggest that during storm surge events the maximum levels increase in whole domain, with the largest increase found for the 100 return period storm surge scenario (1.17 m). The most significant changes occur at the main channels head for all scenarios, revealing that these regions are the most vulnerable to marginal flooding. Also, storm surges induce higher velocities and tidal prisms in the lagoon, increasing the marginal risk of erosion, as well as the salinization of the lagoon marginal lands.pt_PT
dc.language.isoengpt_PT
dc.publisherCoastal Education and Research Foundationpt_PT
dc.relationinfo:eu-repo/grantAgreement/FCT/SFRH/SFRH%2FBD%2F79920%2F2011/PTpt_PT
dc.relationinfo:eu-repo/grantAgreement/FCT/SFRH/SFRH%2FBD%2F78345%2F2011/PTpt_PT
dc.relationinfo:eu-repo/grantAgreement/FCT/SFRH/SFRH%2FBD%2F79555%2F2011/PTpt_PT
dc.relationinfo:eu-repo/grantAgreement/FCT/5876-PPCDTI/100953/PTpt_PT
dc.relationinfo:eu-repo/grantAgreement/FCT/5876-PPCDTI/107939/PTpt_PT
dc.relationinfo:eu-repo/grantAgreement/FCT/COMPETE/121191/PTpt_PT
dc.rightsrestrictedAccesspt_PT
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/pt_PT
dc.titleStorm surge impact in the hydrodynamics of a tidal lagoon: the case of Ria de Aveiropt_PT
dc.typearticlept_PT
dc.description.versionpublishedpt_PT
dc.peerreviewedyespt_PT
degois.publication.firstPage796pt_PT
degois.publication.issue65pt_PT
degois.publication.lastPage801pt_PT
degois.publication.titleJournal of Coastal Researchpt_PT
degois.publication.volume1pt_PT
dc.relation.publisherversionhttp://www.bioone.org/doi/10.2112/SI65-135.1pt_PT
dc.identifier.doi10.2112/SI65-135.1pt_PT
dc.identifier.essn1551-5036pt_PT
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