Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/38026
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dc.contributor.authorSwain, J-
dc.date.accessioned2016-12-01T10:25:49Z-
dc.date.available2016-12-01T10:25:49Z-
dc.date.issued1992-06-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/38026-
dc.description89-98en_US
dc.description.abstractA new parameter R(pz) is proposed for overall composition of a given sea-state as seas and swells. R(pz) is the ratio between computed peak period using Kruseman's mean wind wave spectrum and observed zero-upcrossing period or significant period of waves (visual/observed). Wind speed, significant wave height and period derived through zero-upcrossing and spectral analysis are used to compute R(pz) and their comparison reveals a better agreement. The proposed parameter is compared with few commonly used parameters available in the literature for estimating sea-state composition or spectral behaviour of waves. The present analysis suggests that, R(pz) is a better parameter to describe sea-state composition for a variety of wind-wave conditions which consists of either single-peaked or multi-peaked wave spectra.en_US
dc.language.isoen_USen_US
dc.publisherNISCAIR-CSIR, Indiaen_US
dc.rights CC Attribution-Noncommercial-No Derivative Works 2.5 Indiaen_US
dc.sourceIJMS Vol.21(2) [June 1992]en_US
dc.titleApplication of Kruseman's mean wind wave spectrum for sea-state compositionen_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.21(2) [June 1992]

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