Please use this identifier to cite or link to this item: http://repositorio.lnec.pt:8080/jspui/handle/123456789/1009976
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dc.contributor.authorMendes, D.pt_BR
dc.contributor.authorPinto, J. P.pt_BR
dc.contributor.authorPires Silva, A.pt_BR
dc.contributor.authorFortunato, A. B.pt_BR
dc.date.accessioned2017-10-30T12:39:54Zpt_BR
dc.date.accessioned2018-03-06T16:22:36Z-
dc.date.available2017-10-30T12:39:54Zpt_BR
dc.date.available2018-03-06T16:22:36Z-
dc.date.issued2017-06pt_BR
dc.identifier.urihttps://repositorio.lnec.pt/jspui/handle/123456789/1009976-
dc.description.abstractField observations were performed at an embayed beachto investigate infragravity (IG) wave (0.005-0.04 Hz) dynamics. Offshore short-wave conditions measured by the Cabo Sillero buoy (323 m depth) were characterized by a mean significant wave height of 0.9 m and a mean peak wave period of 9 s. Analysis of field observations demonstrate that for this embayed beach two IG wave peaks can be detected (0.01 and 0.025 Hz). The IG wave band can be separated in two frequency bands due to the different wave propagation characteristics (0.005-0.02 and 0.02-0.04 Hz). The bound wave generation mechanism was identified based on a negative correlation between the short-wave envelope and the IG wave elevation for a time lag of 5 s. The phase-lag evolution of the IG wave increasingly lags behind the short-wave envelope shorewards.pt_BR
dc.language.isoengpt_BR
dc.publisherNão disponivelpt_BR
dc.rightsopenAccesspt_BR
dc.subjectBound wavept_BR
dc.subjectPhase-lag evolutionpt_BR
dc.subjectField measurementspt_BR
dc.subjectCross-spectral analysispt_BR
dc.titleInfragravity wave dynamics on an embayed beachpt_BR
dc.typeconferenceObjectpt_BR
dc.description.pages389-398pppt_BR
dc.description.sectorDHA/NECpt_BR
dc.description.magazineProceedings of Coastal Dynamics 2017pt_BR
dc.contributor.peer-reviewedNAOpt_BR
dc.contributor.academicresearchersNAOpt_BR
dc.contributor.arquivoSIMpt_BR
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