A preliminary laboratory study of motion of floating debris generated by solitary waves running up a beach

Destructive tsunamis can destroy coastal structures and move huge amounts of tsunami debris. Our current understanding of motion of tsunami debris in tsunami flows is limited. In this paper, we present a preliminary laboratory study of motion of model debris under the action of solitary waves runnin...

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Main Authors: Shen, Hung-Tao, Huang, Zhenhua, Yao, Yao, Lo, Edmond Yat Man
Other Authors: School of Civil and Environmental Engineering
Format: Article
Language:English
Published: 2014
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Online Access:https://hdl.handle.net/10356/101979
http://hdl.handle.net/10220/24224
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Institution: Nanyang Technological University
Language: English
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spelling sg-ntu-dr.10356-1019792020-09-26T21:32:31Z A preliminary laboratory study of motion of floating debris generated by solitary waves running up a beach Shen, Hung-Tao Huang, Zhenhua Yao, Yao Lo, Edmond Yat Man School of Civil and Environmental Engineering Institute of Catastrophe Risk Management Earth Observatory of Singapore DRNTU::Engineering::Civil engineering::Water resources Destructive tsunamis can destroy coastal structures and move huge amounts of tsunami debris. Our current understanding of motion of tsunami debris in tsunami flows is limited. In this paper, we present a preliminary laboratory study of motion of model debris under the action of solitary waves running up a beach. The difference between the waterline of maximum inundation and the final position of debris was examined under various conditions. Effects of solitary wave height, water depth, and the distance of debris source to the shoreline on the maximum inundation, the debris limit, and the final position of debris were examined. In general, the final positions of the debris are different from the waterline at maximum inundation and there is a low possibility that a large amount of debris can be carried by retreating water offshore into the sea. NRF (Natl Research Foundation, S’pore) MOE (Min. of Education, S’pore) Accepted version 2014-11-13T09:06:34Z 2019-12-06T20:47:50Z 2014-11-13T09:06:34Z 2019-12-06T20:47:50Z 2014 2014 Journal Article Yao, Y., Huang, Z., Lo, E. Y. M., & Shen, H.-T. (2014). A preliminary laboratory study of motion of floating debris generated by solitary waves running up a beach. Journal of earthquake and tsunami, 8(3), 1440006-. 1793-4311 https://hdl.handle.net/10356/101979 http://hdl.handle.net/10220/24224 10.1142/S1793431114400065 en Journal of earthquake and tsunami © 2014 World Scientific Publishing Company. This is the author created version of a work that has been peer reviewed and accepted for publication by Journal of Earthquake and Tsunami, World Scientific Publishing Company. It incorporates referee’s comments but changes resulting from the publishing process, such as copyediting, structural formatting, may not be reflected in this document. The published version is available at: [Article DOI: http://dx.doi.org/10.1142/S1793431114400065]. 13 p. application/pdf
institution Nanyang Technological University
building NTU Library
country Singapore
collection DR-NTU
language English
topic DRNTU::Engineering::Civil engineering::Water resources
spellingShingle DRNTU::Engineering::Civil engineering::Water resources
Shen, Hung-Tao
Huang, Zhenhua
Yao, Yao
Lo, Edmond Yat Man
A preliminary laboratory study of motion of floating debris generated by solitary waves running up a beach
description Destructive tsunamis can destroy coastal structures and move huge amounts of tsunami debris. Our current understanding of motion of tsunami debris in tsunami flows is limited. In this paper, we present a preliminary laboratory study of motion of model debris under the action of solitary waves running up a beach. The difference between the waterline of maximum inundation and the final position of debris was examined under various conditions. Effects of solitary wave height, water depth, and the distance of debris source to the shoreline on the maximum inundation, the debris limit, and the final position of debris were examined. In general, the final positions of the debris are different from the waterline at maximum inundation and there is a low possibility that a large amount of debris can be carried by retreating water offshore into the sea.
author2 School of Civil and Environmental Engineering
author_facet School of Civil and Environmental Engineering
Shen, Hung-Tao
Huang, Zhenhua
Yao, Yao
Lo, Edmond Yat Man
format Article
author Shen, Hung-Tao
Huang, Zhenhua
Yao, Yao
Lo, Edmond Yat Man
author_sort Shen, Hung-Tao
title A preliminary laboratory study of motion of floating debris generated by solitary waves running up a beach
title_short A preliminary laboratory study of motion of floating debris generated by solitary waves running up a beach
title_full A preliminary laboratory study of motion of floating debris generated by solitary waves running up a beach
title_fullStr A preliminary laboratory study of motion of floating debris generated by solitary waves running up a beach
title_full_unstemmed A preliminary laboratory study of motion of floating debris generated by solitary waves running up a beach
title_sort preliminary laboratory study of motion of floating debris generated by solitary waves running up a beach
publishDate 2014
url https://hdl.handle.net/10356/101979
http://hdl.handle.net/10220/24224
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