Instability of surface shear layer induced by wind

Please use this identifier to cite or link to this item: https://scholarbank.nus.edu.sg/handle/10635/58406

DC Field	Value
dc.title	Instability of surface shear layer induced by wind
dc.contributor.author	Zhang, Q.D.
dc.contributor.author	Yeo, K.S.
dc.contributor.author	Khoo, B.C.
dc.date.accessioned	2014-06-17T05:14:14Z
dc.date.available	2014-06-17T05:14:14Z
dc.date.issued	1995-12
dc.identifier.citation	Zhang, Q.D.,Yeo, K.S.,Khoo, B.C. (1995-12). Instability of surface shear layer induced by wind. International Journal of Offshore and Polar Engineering 5 (4) : 273-278. ScholarBank@NUS Repository.
dc.identifier.issn	10535381
dc.identifier.uri	http://scholarbank.nus.edu.sg/handle/10635/58406
dc.description.abstract	By the numerical solution of the Rayleigh equation for complex frequency and complex wave number, the stability of four families of surface shear flow, which represent velocity profiles induced by wind over a water surface, has been investigated. It is shown that for flow of Froude number from 0.85 to 1.41, the unstable waves are primarily convective in nature.
dc.source	Scopus
dc.type	Article
dc.contributor.department	MECHANICAL & PRODUCTION ENGINEERING
dc.description.sourcetitle	International Journal of Offshore and Polar Engineering
dc.description.volume	5
dc.description.issue	4
dc.description.page	273-278
dc.description.coden	IOPEE
dc.identifier.isiut	NOT_IN_WOS
Appears in Collections:	Staff Publications

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