Impulse Wave Runup on Steep to Vertical Slopes

Impulse waves are generated by landslides or avalanches impacting oceans, lakes or reservoirs, for example. Non-breaking impulse wave runup on slope angles ranging from 10° to 90° (V/H: 1/5.7 to 1/0) is investigated. The prediction of runup heights induced by these waves is an import...

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Main Authors: Frederic M. Evers, Robert M. Boes
Format: Article
Language:English
Published: MDPI AG 2019-01-01
Series:Journal of Marine Science and Engineering
Subjects:
Online Access:http://www.mdpi.com/2077-1312/7/1/8
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spelling doaj-9f9f9c25322046dda349c615587adbd12021-04-02T04:27:13ZengMDPI AGJournal of Marine Science and Engineering2077-13122019-01-0171810.3390/jmse7010008jmse7010008Impulse Wave Runup on Steep to Vertical SlopesFrederic M. Evers0Robert M. Boes1Laboratory of Hydraulics, Hydrology and Glaciology (VAW), ETH Zurich, CH-8093 Zürich, SwitzerlandLaboratory of Hydraulics, Hydrology and Glaciology (VAW), ETH Zurich, CH-8093 Zürich, SwitzerlandImpulse waves are generated by landslides or avalanches impacting oceans, lakes or reservoirs, for example. Non-breaking impulse wave runup on slope angles ranging from 10° to 90° (V/H: 1/5.7 to 1/0) is investigated. The prediction of runup heights induced by these waves is an important parameter for hazard assessment and mitigation. An experimental dataset containing 359 runup heights by impulse and solitary waves is compiled from several published sources. Existing equations, both empirical and analytical, are then applied to this dataset to assess their prediction quality on an extended parameter range. Based on this analysis, a new prediction equation is proposed. The main findings are: (1) solitary waves are a suitable proxy for modelling impulse wave runup; (2) commonly applied equations from the literature may underestimate the runup height of small wave amplitudes; (3) the proposed semi-empirical equations predict the overall dataset within ±20% scatter for relative wave crest amplitudes ε, i.e., the wave crest amplitude normalised with the stillwater depth, between 0.007 and 0.69.http://www.mdpi.com/2077-1312/7/1/8impulse wavesolitary wavelandslide tsunamiwave runuprunup prediction
collection DOAJ
language English
format Article
sources DOAJ
author Frederic M. Evers
Robert M. Boes
spellingShingle Frederic M. Evers
Robert M. Boes
Impulse Wave Runup on Steep to Vertical Slopes
Journal of Marine Science and Engineering
impulse wave
solitary wave
landslide tsunami
wave runup
runup prediction
author_facet Frederic M. Evers
Robert M. Boes
author_sort Frederic M. Evers
title Impulse Wave Runup on Steep to Vertical Slopes
title_short Impulse Wave Runup on Steep to Vertical Slopes
title_full Impulse Wave Runup on Steep to Vertical Slopes
title_fullStr Impulse Wave Runup on Steep to Vertical Slopes
title_full_unstemmed Impulse Wave Runup on Steep to Vertical Slopes
title_sort impulse wave runup on steep to vertical slopes
publisher MDPI AG
series Journal of Marine Science and Engineering
issn 2077-1312
publishDate 2019-01-01
description Impulse waves are generated by landslides or avalanches impacting oceans, lakes or reservoirs, for example. Non-breaking impulse wave runup on slope angles ranging from 10° to 90° (V/H: 1/5.7 to 1/0) is investigated. The prediction of runup heights induced by these waves is an important parameter for hazard assessment and mitigation. An experimental dataset containing 359 runup heights by impulse and solitary waves is compiled from several published sources. Existing equations, both empirical and analytical, are then applied to this dataset to assess their prediction quality on an extended parameter range. Based on this analysis, a new prediction equation is proposed. The main findings are: (1) solitary waves are a suitable proxy for modelling impulse wave runup; (2) commonly applied equations from the literature may underestimate the runup height of small wave amplitudes; (3) the proposed semi-empirical equations predict the overall dataset within ±20% scatter for relative wave crest amplitudes ε, i.e., the wave crest amplitude normalised with the stillwater depth, between 0.007 and 0.69.
topic impulse wave
solitary wave
landslide tsunami
wave runup
runup prediction
url http://www.mdpi.com/2077-1312/7/1/8
work_keys_str_mv AT fredericmevers impulsewaverunuponsteeptoverticalslopes
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