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Experimental results of wave transformation across a sloping beach

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dc.contributor.author Memos Constantine, D en
dc.date.accessioned 2014-03-01T02:48:20Z
dc.date.available 2014-03-01T02:48:20Z
dc.date.issued 1995 en
dc.identifier.issn 08938717 en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/33735
dc.relation.uri http://www.scopus.com/inward/record.url?eid=2-s2.0-0029216829&partnerID=40&md5=e063c07e7783c0453c7730931ef8aa57 en
dc.subject.other Beaches en
dc.subject.other Coastal zones en
dc.subject.other Correlation methods en
dc.subject.other Mathematical models en
dc.subject.other Probability en
dc.subject.other Wave transmission en
dc.subject.other Sea bed en
dc.subject.other Sloping beach en
dc.subject.other Surf zone en
dc.subject.other Wave transformation en
dc.subject.other Water waves en
dc.title Experimental results of wave transformation across a sloping beach en
heal.type conferenceItem en
heal.publicationDate 1995 en
heal.abstract Experiments have been conducted to investigate the transformations of the wave characteristics induced by a uniformly decreasing sea bed. These transformations were recorded on both the frequency and the time domain representations of random wave trains. The coastal zone upwind of severe breaking was studied. Among the findings it is noted the tendency of the spectrum width parameter to decrease at a slowing rate as the waves propagate on shoaling waters. Also, the correlation coefficient between wave heights and periods seems to inversely follow the variations of a measure of the wave heights. A mathematical model has been developed based on existing results for shoaling, wave breaking and decay. This model applicable to a wide area of the surf zone predicts adequately the evolution of the joint probability between wave heights and periods provided by the experimental results. en
heal.publisher ASCE, New York, NY, United States en
heal.journalName Proceedings of the Coastal Engineering Conference en
dc.identifier.volume 2 en
dc.identifier.spage 2350 en
dc.identifier.epage 2364 en


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