An experimental study of the surface drift currents in a wave flume

The Lagrangian surface drift current induced by surface gravity waves in a wave flume has been investigated experimentally by the particle tracking method. It was observed that in most regions of the flume, the time-mean surface drift current was in the opposite direction to that of the wave propaga...

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Bibliographic Details
Main Author: Huang, Zhenhua
Other Authors: School of Civil and Environmental Engineering
Format: Journal Article
Language:English
Published: 2013
Subjects:
Online Access:https://hdl.handle.net/10356/97492
http://hdl.handle.net/10220/10527
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author Huang, Zhenhua
author2 School of Civil and Environmental Engineering
author_facet School of Civil and Environmental Engineering
Huang, Zhenhua
author_sort Huang, Zhenhua
collection NTU
description The Lagrangian surface drift current induced by surface gravity waves in a wave flume has been investigated experimentally by the particle tracking method. It was observed that in most regions of the flume, the time-mean surface drift current was in the opposite direction to that of the wave propagation. The secondary current in the form of a pair of longitudinal vortices caused by the lateral boundaries was analyzed. It is suggested that the convection of the vorticity generated by the wave-absorber and the lateral boundaries is an important factor in the determination of the time-mean drift in a wave flume.
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spelling ntu-10356/974922020-03-07T11:43:44Z An experimental study of the surface drift currents in a wave flume Huang, Zhenhua School of Civil and Environmental Engineering DRNTU::Social sciences::Geography::Oceanography The Lagrangian surface drift current induced by surface gravity waves in a wave flume has been investigated experimentally by the particle tracking method. It was observed that in most regions of the flume, the time-mean surface drift current was in the opposite direction to that of the wave propagation. The secondary current in the form of a pair of longitudinal vortices caused by the lateral boundaries was analyzed. It is suggested that the convection of the vorticity generated by the wave-absorber and the lateral boundaries is an important factor in the determination of the time-mean drift in a wave flume. 2013-06-21T07:07:21Z 2019-12-06T19:43:16Z 2013-06-21T07:07:21Z 2019-12-06T19:43:16Z 2006 2006 Journal Article Huang, Z. (2007). An experimental study of the surface drift currents in a wave flume. Ocean Engineering, 34(2), 343-352. 0029-8018 https://hdl.handle.net/10356/97492 http://hdl.handle.net/10220/10527 10.1016/j.oceaneng.2006.01.005 en Ocean engineering © 2006 Elsevier Ltd.
spellingShingle DRNTU::Social sciences::Geography::Oceanography
Huang, Zhenhua
An experimental study of the surface drift currents in a wave flume
title An experimental study of the surface drift currents in a wave flume
title_full An experimental study of the surface drift currents in a wave flume
title_fullStr An experimental study of the surface drift currents in a wave flume
title_full_unstemmed An experimental study of the surface drift currents in a wave flume
title_short An experimental study of the surface drift currents in a wave flume
title_sort experimental study of the surface drift currents in a wave flume
topic DRNTU::Social sciences::Geography::Oceanography
url https://hdl.handle.net/10356/97492
http://hdl.handle.net/10220/10527
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