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contributor authorR. C. Ertekin
contributor authorY. Z. Liu
contributor authorB. Padmanabhan
date accessioned2017-05-08T23:45:14Z
date available2017-05-08T23:45:14Z
date copyrightNovember, 1994
date issued1994
identifier issn0892-7219
identifier otherJMOEEX-28096#214_1.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/114176
description abstractA linear ray theory is developed to study the interaction of water waves with a steady intake-pipe flow in deep water. The wave-current interaction model is based on the assumption that the current field is slowly varying in comparison with the wave field. With the use of the dispersion relation, an equation is derived for the wave number that also depends on the current velocity field. Imposing the condition of irrotationality of wave number, a nonlinear set of characteristic equations of oblique waves is obtained and solved numerically to determine the rays. The current field is generated by solving the 3-D potential problem of specified intake normal-velocity at the entrance of a horizontal, circular pipe of semi-infinite length, situated on the still-water level, by using the axisymmetric Rankine source method. It appears that the velocity-potential solution of the intake-pipe flow problem presented here does not exist in the literature. Finally, the local wave amplitudes are calculated through the conservation of wave-action equation to predict the focusing of wave energy.
publisherThe American Society of Mechanical Engineers (ASME)
titleInteraction of Incoming Waves With a Steady Intake-Pipe Flow
typeJournal Paper
journal volume116
journal issue4
journal titleJournal of Offshore Mechanics and Arctic Engineering
identifier doi10.1115/1.2920154
journal fristpage214
journal lastpage220
identifier eissn1528-896X
keywordsFlow (Dynamics)
keywordsWaves
keywordsPipes
keywordsEquations
keywordsWater
keywordsWave energy
keywordsDispersion relations AND Water waves
treeJournal of Offshore Mechanics and Arctic Engineering:;1994:;volume( 116 ):;issue: 004
contenttypeFulltext


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