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Wave transformation on shore platform and adjacent sandy beach - Southern Portugal

dc.contributor.authorGabriel, Selma
dc.contributor.authorMoura, Delminda
dc.contributor.authorHorta, João
dc.contributor.authorOliveira, Sónia
dc.date.accessioned2013-03-01T15:46:21Z
dc.date.available2013-03-01T15:46:21Z
dc.date.issued2012
dc.description.abstractThe knowledge on coastal processes is not only of basic and practical importance (for instance in engineering applications) but also of socio-economic relevance. Crenulated coasts are complex geomorphic environments where both erosive (into headlands) and depositional processes (in embayed beaches) occur simultaneously. Waves represent an important morphogenic factor and the most important source of energy to coastal zones. However, field data reporting the interaction between waves and rocky coastal features is still scarce, leading to a poor understanding on rates and drivers of surf attenuation at rocky shores. Waves abrasion and erosion on shore platforms depend on the platform properties, morphology of the adjacent continental shelf, and water depth upon the platform surface, which is controlled by tides, available sediment and wave climate (e.g.,Stephenson and Kirk, 2000; Marshall and Stephenson, 2011). Shore platforms extending in the intertidal zone at the rocky cliffs’ toe are natural morphological barriers to wave propagation and energy attenuation (Ogawa et al., 2011). Over short time scales the beaches in a crenulated coast are modified mainly by waves causing setup and set down in the surf zone leading to a very complex pattern and circulation modified by the interaction between the currents induced by waves and the incident waves. The mechanisms involved in morphological modifications in those environments are still not well understood (Silva et al., 2010). This work aims to compare the waves behavior both on a shore platform and adjacent pocket beach in response to exactly the same offshore wave conditions.por
dc.description.sponsorshipThis work was supported by a grant SFRH/BD/64497/2009, and is a contribution for the research project PTDC/CTEGIX/111230/2009 both supported by Portuguese Foundation for Science and Technology (FCT).por
dc.identifier.isbn978-90-382-2008-6
dc.identifier.otherAUT: DMO00293;
dc.identifier.urihttp://hdl.handle.net/10400.1/2519
dc.language.isoengpor
dc.peerreviewedyespor
dc.relationPLATAFORMAS ROCHOSAS VERSUS PRAIAS ARENOSAS: QUAL EXERCE MAIOR PROTECÇÃO RELATIVAMENTE AO RECUO NATURAL DE UMA ARRIBA
dc.subjectWave transformationpor
dc.subjectShore platformpor
dc.subjectBeachpor
dc.titleWave transformation on shore platform and adjacent sandy beach - Southern Portugalpor
dc.typeconference object
dspace.entity.typePublication
oaire.awardTitlePLATAFORMAS ROCHOSAS VERSUS PRAIAS ARENOSAS: QUAL EXERCE MAIOR PROTECÇÃO RELATIVAMENTE AO RECUO NATURAL DE UMA ARRIBA
oaire.awardURIinfo:eu-repo/grantAgreement/FCT//SFRH%2FBD%2F64497%2F2009/PT
oaire.citation.conferencePlaceGhent, Belgiumpor
oaire.citation.endPage171por
oaire.citation.startPage169por
oaire.citation.titleCoastlab 12, Fourth International Conference on the Application of Physical Modelling to Port and Coastal Protectionpor
person.familyNameMoura
person.familyNameHorta
person.familyNameJenkins Oliveira Fernandes
person.givenNameDelminda
person.givenNameJoão
person.givenNameSónia Alexandra
person.identifier.ciencia-id7B1C-1CB3-A37D
person.identifier.orcid0000-0002-0952-6805
person.identifier.orcid0000-0003-3663-9036
person.identifier.orcid0000-0002-2991-686X
person.identifier.scopus-author-id15048413000
person.identifier.scopus-author-id55851149800
person.identifier.scopus-author-id57193909844
project.funder.identifierhttp://doi.org/10.13039/501100001871
project.funder.nameFundação para a Ciência e a Tecnologia
rcaap.rightsopenAccesspor
rcaap.typeconferenceObjectpor
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relation.isAuthorOfPublication166f1a46-251d-4cd2-b753-7f50ee0439c0
relation.isAuthorOfPublication64412170-4564-4615-8fe0-d6e681015efa
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