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Ocean depth effects on tsunami amplitudes used in source models in linearized shallow-water wave theory

dc.contributor.authorHayir, Abdul
dc.contributor.ituauthorHayır, Abdul
dc.date.accessioned2026-01-26T08:21:06Z
dc.date.issued2004-02-01
dc.description.abstractAbstract The aim of this study is to determine the effects of ocean depth on tsunami amplitudes used in source models for use in linear shallow-water wave theory. To determine the effects, 19 ocean depths ranging from 200–2000 m are studied. The results show that it is possible to establish a series-type exploration function to define the depth-amplitude effects. This function with the unknown coefficients related to ruptures of the ocean floor involves the normalized maximum tsunami amplitude. Results obtained from this series-function give good approximations for four or more terms in the series. Two basic source models are considered. Numerical examples are presented.
dc.description.urihttps://doi.org/10.1016/j.oceaneng.2003.07.005
dc.description.urihttps://dx.doi.org/10.1016/j.oceaneng.2003.07.005
dc.identifier.doi10.1016/j.oceaneng.2003.07.005
dc.identifier.endpage361
dc.identifier.issn0029-8018
dc.identifier.openairedoi_dedup___::fbcc32a86a2a6b9314bef0b95211bcc5
dc.identifier.orcid0000-0001-7498-4629
dc.identifier.startpage353
dc.identifier.urihttps://hdl.handle.net/11527/64379
dc.identifier.volume31
dc.language.isoeng
dc.publisherElsevier BV
dc.relation.ispartofOcean Engineering
dc.rightsCLOSED
dc.sdg.typeGoal 14: Life Below Water
dc.titleOcean depth effects on tsunami amplitudes used in source models in linearized shallow-water wave theory
dc.typeArticle
dspace.entity.typePublication
person.identifier.orcid0000-0001-7498-4629

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