Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/38362
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dc.contributor.authorVatkey, M J-
dc.date.accessioned2016-12-09T05:44:31Z-
dc.date.available2016-12-09T05:44:31Z-
dc.date.issued1989-09-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/38362-
dc.description177-183en_US
dc.description.abstractIt is known that the phases of the individual harmonic components in a linear narrow band wave spectrum are uniformly random. It has been suggested by some workers that some sort of phase coupling and `locking' between the different spectral components would lead to nonlinear surface waves. Conventional methods of wave recording and analysis inherently fail to record or to bring out the exact quantitative picture of nonlinear interactions due to recording and sampling limitations in relation to nonlinear waves with vertical and horizontal asymmetries especially in the case of breaking and shoaling waves. Hence, the inverse method of computing the surface profile from a known autospectrum using transformed (tuned) phase spectrum with coupling of different natures is tried and the results are presented here. Increased wave groupiness is found for higher spectral peak periods with phase coherency at the peak. Abnormally high breaking waves (freak waves) are generated when frequency dependent (by Normal probability law) phase spectrum is used. The results suggest that external factors like currents, wind, boundaries (bottom) and other waves systems can cause changes in the phase spectrum to give rise to nonlinear processes.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.18(3) [September 1989]en_US
dc.titleNumerical simulation of wind wave surface profiles with tuned phase spectraen_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.18(3) [September 1989]

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