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dc.contributor.authorValentin Heller
dc.contributor.authorMahtab Moalemi
dc.contributor.authorRobert D. Kinnear
dc.contributor.authorRorik A. Adams
dc.date.accessioned2017-05-08T22:04:10Z
dc.date.available2017-05-08T22:04:10Z
dc.date.copyrightJuly 2012
dc.date.issued2012
dc.identifier.other%28asce%29ww%2E1943-5460%2E0000176.pdf
dc.identifier.urihttp://yetl.yabesh.ir/yetl/handle/yetl/70412
dc.description.abstractLandslide-generated tsunami predictions are commonly based on two-dimensional (2D) wave channel or three-dimensional (3D) wave basin experiments with considerably different outcomes. It is not fully understood which idealized water body geometry applies best to a specific prototype. Hence, a physical small-scale model study has been conducted that, for the first time, systematically investigates the effect of geometry on landslide-generated tsunami height, amplitude, period, and celerity. A rigid slide generated tsunamis propagating in various geometries characterized by the basin side angle
dc.publisherAmerican Society of Civil Engineers
dc.titleGeometrical Effects on Landslide-Generated Tsunamis
dc.typeJournal Paper
dc.journal.volume138
dc.journal.issue4
dc.journal.titleJournal of Waterway, Port, Coastal, and Ocean Engineering
dc.identifier.doi10.1061/(ASCE)WW.1943-5460.0000130
dc.treeJournal of Waterway, Port, Coastal, and Ocean Engineering:;2012:;Volume ( 138 ):;issue: 004
dc.contenttypeFulltext


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