Abstract
Nearshore rhythmicity is often initiated in the period just after a storm where the subtidal bar is turned alongshore uniform. The initiation time as well as the length scales of the created rhythmicity varies from one storm period to another. Here we show that the post-storm wave conditions are related to the initiation of the morphological rhythmicity. Narrow-banded and long wave period, both proxies for swell waves, are often found to be present prior to the initiation of rhythmicity. Furthermore, numerical model computations illustrate that swell waves induce significantly larger wave group induced velocities on the bar. These findings imply that the arrival of swell waves can initiate and stimulate the nearshore morphological rhythmicity.
Original language | English |
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Title of host publication | Proceedings of 32nd Conference on Coastal Engineering, ICCE 2010 |
Editors | J McKee Smith, P Lynett |
Place of Publication | s.l. |
Publisher | s.n. |
Pages | 1-14 |
Number of pages | 14 |
DOIs | |
Publication status | Published - 2011 |
Event | 32nd International Conference on Coastal Engineering - s.l., Shanghai, China Duration: 30 Jun 2010 → 5 Jul 2010 Conference number: 32 |
Publication series
Name | Coastal Engineering Proceedings |
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Number | 32 |
Conference
Conference | 32nd International Conference on Coastal Engineering |
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Abbreviated title | ICCE 2010 |
Country/Territory | China |
City | Shanghai |
Period | 30/06/10 → 5/07/10 |
Bibliographical note
geen ISBNKeywords
- Nearshore sandbars
- Rhythmicity
- Wave groups