Two- and three-dimensional computation of solitary wave runup on non-plane beach
DC Field | Value | Language |
---|---|---|
dc.contributor.author | Choi, BH[Choi, B. H.] | - |
dc.contributor.author | Pelinovsky, E[Pelinovsky, E.] | - |
dc.contributor.author | Kim, DC[Kim, D. C.] | - |
dc.contributor.author | Didenkulova, I[Didenkulova, I.] | - |
dc.contributor.author | Woo, SB[Woo, S. -B.] | - |
dc.date.accessioned | 2021-08-07T20:43:13Z | - |
dc.date.available | 2021-08-07T20:43:13Z | - |
dc.date.created | 2016-10-20 | - |
dc.date.issued | 2008 | - |
dc.identifier.issn | 1023-5809 | - |
dc.identifier.uri | https://scholarworks.bwise.kr/skku/handle/2021.sw.skku/83234 | - |
dc.description.abstract | Solitary wave runup on a non-plane beach is studied analytically and numerically. For the theoretical approach, nonlinear shallow-water theory is applied to obtain the analytical solution for the simplified bottom geometry, such as an inclined channel whose cross-slope shape is parabolic. It generalizes Carrier-Greenspan approach for long wave runup on the inclined plane beach that is currently used now. For the numerical study, the Reynolds Averaged Navier-Stokes (RANS) system is applied to study soliton runup on an inclined beach and the detailed characteristics of the wave processes (water displacement, velocity field, turbulent kinetic energy, energy dissipation) are analyzed. In this study, it is theoretically and numerically proved that the existence of a parabolic cross-slope channel on the plane beach causes runup intensification, which is often observed in post-tsunami field surveys. | - |
dc.publisher | COPERNICUS GESELLSCHAFT MBH | - |
dc.subject | VERTICAL WALL | - |
dc.subject | SLOPING BEACH | - |
dc.subject | LONG WAVES | - |
dc.subject | TSUNAMI | - |
dc.subject | AMPLITUDE | - |
dc.subject | EVOLUTION | - |
dc.subject | ISLAND | - |
dc.subject | FLOWS | - |
dc.title | Two- and three-dimensional computation of solitary wave runup on non-plane beach | - |
dc.type | Article | - |
dc.contributor.affiliatedAuthor | Choi, BH[Choi, B. H.] | - |
dc.contributor.affiliatedAuthor | Kim, DC[Kim, D. C.] | - |
dc.identifier.wosid | 000257304300011 | - |
dc.identifier.bibliographicCitation | NONLINEAR PROCESSES IN GEOPHYSICS, v.15, no.3, pp.489 - 502 | - |
dc.relation.isPartOf | NONLINEAR PROCESSES IN GEOPHYSICS | - |
dc.citation.title | NONLINEAR PROCESSES IN GEOPHYSICS | - |
dc.citation.volume | 15 | - |
dc.citation.number | 3 | - |
dc.citation.startPage | 489 | - |
dc.citation.endPage | 502 | - |
dc.type.rims | ART | - |
dc.type.docType | Article | - |
dc.description.journalClass | 1 | - |
dc.description.journalRegisteredClass | scie | - |
dc.description.journalRegisteredClass | scopus | - |
dc.subject.keywordPlus | VERTICAL WALL | - |
dc.subject.keywordPlus | SLOPING BEACH | - |
dc.subject.keywordPlus | LONG WAVES | - |
dc.subject.keywordPlus | TSUNAMI | - |
dc.subject.keywordPlus | AMPLITUDE | - |
dc.subject.keywordPlus | EVOLUTION | - |
dc.subject.keywordPlus | ISLAND | - |
dc.subject.keywordPlus | FLOWS | - |
Items in ScholarWorks are protected by copyright, with all rights reserved, unless otherwise indicated.
(03063) 25-2, SUNGKYUNKWAN-RO, JONGNO-GU, SEOUL, KOREAsamsunglib@skku.edu
COPYRIGHT © 2021 SUNGKYUNKWAN UNIVERSITY ALL RIGHTS RESERVED.
Certain data included herein are derived from the © Web of Science of Clarivate Analytics. All rights reserved.
You may not copy or re-distribute this material in whole or in part without the prior written consent of Clarivate Analytics.