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contributor authorHerman C. Miller
contributor authorC. Linwood Vincent
date accessioned2017-05-08T21:09:24Z
date available2017-05-08T21:09:24Z
date copyrightJanuary 1990
date issued1990
identifier other%28asce%290733-950x%281990%29116%3A1%2857%29.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/40793
description abstractThis paper describes the development of a mathematical function that represents the spectrum of wind‐generated gravity waves in water of arbitrary depth. The derivation parallels that of the TMA spectrum. The primary difference is that Phillips' (1958) model for saturation at high frequencies is replaced by Kitaigorodskii's (1983) model. This spectrum incorporates wind speed directly into the formulation and is consistent with an
publisherAmerican Society of Civil Engineers
titleFRF Spectrum: TMA with Kitaigorodskii's f-4 Scaling
typeJournal Paper
journal volume116
journal issue1
journal titleJournal of Waterway, Port, Coastal, and Ocean Engineering
identifier doi10.1061/(ASCE)0733-950X(1990)116:1(57)
treeJournal of Waterway, Port, Coastal, and Ocean Engineering:;1990:;Volume ( 116 ):;issue: 001
contenttypeFulltext


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