Please use this identifier to cite or link to this item: http://hdl.handle.net/10773/24689
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dc.contributor.authorPereira, Carlapt_PT
dc.contributor.authorCoelho, Carlospt_PT
dc.contributor.authorRibeiro, Alexandrept_PT
dc.contributor.authorFortunato, André B.pt_PT
dc.contributor.authorLopes, Carina L.pt_PT
dc.contributor.authorDias, João M.pt_PT
dc.date.accessioned2018-11-21T15:01:21Z-
dc.date.available2018-11-21T15:01:21Z-
dc.date.issued2013-
dc.identifier.issn0749-0208pt_PT
dc.identifier.urihttp://hdl.handle.net/10773/24689-
dc.description.abstractIn the Northwest coast of Portugal, the shoreline evolution is leading to several problems, such as loss of territory and infrastructural damages, mainly caused by the sea wave’s action. This study aims to predict the impacts of climate change on the shoreline evolution in this coastal area. Coastal stretches studied were Esmoriz-Furadouro and Vagueira- Mira, due to their vulnerability related with the low lying sandy coast, the deficit of sediments, the presence of urban waterfronts and the narrow width of the sand spit that separates the ocean from the Aveiro lagoon. The paper describes the application of two shoreline evolution models (LTC and GENESIS) to the projection of shoreline evolution between 2010 and 2100. A reference scenario considering the present typical wave climate and the mean sea water level was compared with 3 other future scenarios that may result from climate change effects, combining different wave climates and mean sea levels (0.42 and 0.64 m above present level). Considering the numerical models' results, maps of the shoreline position were represented every 30 years. The results allowed the analysis of the shoreline retreat, the areas of lost territory and the alongshore sediment transport volumes in several cross sections. A strong trend of shoreline retreat was found for all the scenarios, although the retreat rates tend to decrease along time. Comparing the reference scenario with the climate change scenarios, a slight clockwise rotation of the shoreline was predicted, also increasing the average shoreline retreat from 6% to 11%, depending on the considered scenario.pt_PT
dc.language.isoengpt_PT
dc.publisherCoastal Education and Research Foundationpt_PT
dc.relationinfo:eu-repo/grantAgreement/FCT/5876-PPCDTI/100953/PTpt_PT
dc.relationinfo:eu-repo/grantAgreement/FCT/SFRH/SFRH%2FBD%2F78345%2F2011/PTpt_PT
dc.rightsrestrictedAccesspt_PT
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/pt_PT
dc.subjectCoastal erosionpt_PT
dc.subjectsea level risept_PT
dc.subjectWave climatept_PT
dc.subjectShoreline retreatpt_PT
dc.subjectErosion ratespt_PT
dc.subjectTerritory lostpt_PT
dc.subjectSediment transportpt_PT
dc.titleNumerical modelling of shoreline evolution in the Aveiro coast, Portugal – climate change scenariospt_PT
dc.typearticlept_PT
dc.description.versionpublishedpt_PT
dc.peerreviewedyespt_PT
degois.publication.firstPage2161pt_PT
degois.publication.issue65pt_PT
degois.publication.lastPage2166pt_PT
degois.publication.titleJournal of Coastal Researchpt_PT
degois.publication.volume2pt_PT
dc.relation.publisherversionhttp://www.bioone.org/doi/10.2112/SI65-365.1pt_PT
dc.identifier.doi10.2112/SI65-365.1pt_PT
dc.identifier.essn1551-5036pt_PT
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