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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Format: | Journal Article |
Language: | English |
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2013
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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. |
first_indexed | 2024-10-01T02:20:29Z |
format | Journal Article |
id | ntu-10356/97492 |
institution | Nanyang Technological University |
language | English |
last_indexed | 2024-10-01T02:20:29Z |
publishDate | 2013 |
record_format | dspace |
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 |
work_keys_str_mv | AT huangzhenhua anexperimentalstudyofthesurfacedriftcurrentsinawaveflume AT huangzhenhua experimentalstudyofthesurfacedriftcurrentsinawaveflume |