Please use this identifier to cite or link to this item: http://ir.lib.seu.ac.lk/handle/123456789/2507
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dc.contributor.authorMuzathik, A.M.-
dc.contributor.authorNik, W.B.Wan-
dc.contributor.authorSamo, K.B.-
dc.contributor.authorIbrahim, M. Z.-
dc.date.accessioned2017-04-24T05:49:23Z-
dc.date.available2017-04-24T05:49:23Z-
dc.date.issued2011-
dc.identifier.citationJournal of Physical Science, 22(1); 79–94.en_US
dc.identifier.issn1675-3402-
dc.identifier.urihttp://ir.lib.seu.ac.lk/handle/123456789/2507-
dc.description.abstractThis paper presents wave measurement and wave climate prediction within Peninsular Malaysia. Rayleigh and Weibull density functions were used to predict wave heights. The total wave energy density was found to be 17.69 MWh/m within an average year, whereas average wave power density varied from 0.15 to 6.49 kW/m. Furthermore, more than 60% of the annual wave energy was caused by wave heights between 0.2 to 1.2 m. Waves with peak periods between 2 and 8 s accounted for more than 70% of the total wave energy. The extreme significant wave heights were predicted, using Gumbel, Weibull and Generalised Pareto distributions, as having return periods of 10 to 200 years for the same locations. The extreme significant wave heights varied from 2.6 to 3.4 m for the aforementioned return periods. The results of the present study will contribute greatly to the design of ocean engineering projects.en_US
dc.language.isoen_USen_US
dc.publisherPenerbit Universiti Sains Malaysiaen_US
dc.subjectGumbelen_US
dc.subjectWeibull and generalised pareto distributionsen_US
dc.subjectSignificant wave heighten_US
dc.subjectWave directionen_US
dc.subjectWave perioden_US
dc.subjectWave energy densityen_US
dc.titleOcean wave measurement and wave climate prediction of peninsular Malaysiaen_US
dc.typeArticleen_US
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