Please use this identifier to cite or link to this item: https://scholarbank.nus.edu.sg/handle/10635/65747
DC FieldValue
dc.titleLaboratory study of deep-water breaking waves
dc.contributor.authorKway, J.H.L.
dc.contributor.authorLoh, Y.-S.
dc.contributor.authorChan, E.-S.
dc.date.accessioned2014-06-17T08:20:11Z
dc.date.available2014-06-17T08:20:11Z
dc.date.issued1998-08
dc.identifier.citationKway, J.H.L., Loh, Y.-S., Chan, E.-S. (1998-08). Laboratory study of deep-water breaking waves. Ocean Engineering 25 (8) : 657-676. ScholarBank@NUS Repository.
dc.identifier.issn00298018
dc.identifier.urihttp://scholarbank.nus.edu.sg/handle/10635/65747
dc.description.abstractIn an attempt to elucidate the mechanics of deep-water wave breaking, a variety of breaking waves, including spilling and plunging waves, of different length scales and geometries was studied. The waves were generated through wave-wave interactions using wave packets with constant-steepness components, constant-amplitude components, and also components following the Pierson-Moskowitz distribution. Wave steepening prior to breaking were found to cause an increase in the high frequency spectral slope of the wave spectrum. The slopes were correlated to the type of breaking and the intensity of the breaking. The energy loss through breaking varied with the spectral characteristics of the wave packet. On the other hand, it was also noted that, irrespective of the wave packet, the losses were from the higher frequency end of the first harmonics. © 1998 Elsevier Science Ltd. All rights reserved.
dc.sourceScopus
dc.typeArticle
dc.contributor.departmentCIVIL ENGINEERING
dc.description.sourcetitleOcean Engineering
dc.description.volume25
dc.description.issue8
dc.description.page657-676
dc.identifier.isiutNOT_IN_WOS
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