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contributor authorArved J. Raudkivi
date accessioned2017-05-08T20:45:21Z
date available2017-05-08T20:45:21Z
date copyrightDecember 2006
date issued2006
identifier other%28asce%290733-9429%282006%29132%3A12%281316%29.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/26040
description abstractThe bed forms generated by the flow of water over alluvial beds are predominantly treated in terms of stability concepts. These generally postulate a constant wavelength, and describe the variation of amplitude. Yet, the wavelength is one of the most variable parameters of these features. The features are also described as ripples, dunes, and antidunes. But there is no explanation on how ripples transform into dunes. On the basis of available data, this paper offers a description of the generation of ripples and their transformation into dunes.
publisherAmerican Society of Civil Engineers
titleTransition from Ripples to Dunes
typeJournal Paper
journal volume132
journal issue12
journal titleJournal of Hydraulic Engineering
identifier doi10.1061/(ASCE)0733-9429(2006)132:12(1316)
treeJournal of Hydraulic Engineering:;2006:;Volume ( 132 ):;issue: 012
contenttypeFulltext


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