1993년 홋카이도 남서 지진에 의한 오쿠시리 섬에서의 지진해일 극한 처오름 산정
DC Field | Value | Language |
---|---|---|
dc.contributor.author | 김동철 | - |
dc.contributor.author | 최병호 | - |
dc.contributor.author | 김경옥 | - |
dc.date.accessioned | 2020-07-16T06:50:15Z | - |
dc.date.available | 2020-07-16T06:50:15Z | - |
dc.date.created | 2020-02-11 | - |
dc.date.issued | 2013-11-21 | - |
dc.identifier.uri | https://sciwatch.kiost.ac.kr/handle/2020.kiost/26528 | - |
dc.description.abstract | This study is based on a series of threedimensional numerical modeling experiments tounderstand the extreme tsunami run-up atMonai valley in Okushiri island, west sea ofJapan caused by the 1993 Hokkaido Nansei-Okiearthquake. The analysis was performed for theextreme run-up height and field observationdata using the run-up height for verification ofmodeling experimental results. As a result, incase of the two island present condition ? realtopography ? extreme run-up height reached toabout 32m (31.7m by observed), so numericalmodel experiment results can be said to be ingood agreement with the observed extremerun-up height. | - |
dc.description.uri | 2 | - |
dc.language | Korean | - |
dc.publisher | 한국해안해양공학회 | - |
dc.relation.isPartOf | 한국해안해양공학회추계학회 | - |
dc.title | 1993년 홋카이도 남서 지진에 의한 오쿠시리 섬에서의 지진해일 극한 처오름 산정 | - |
dc.title.alternative | Extreme tsunami runup simulation at Okushiri due to the 1993 Southwest of Hokkaido earthquake tsunami | - |
dc.type | Conference | - |
dc.citation.conferencePlace | KO | - |
dc.citation.endPage | 73 | - |
dc.citation.startPage | 72 | - |
dc.citation.title | 한국해안해양공학회추계학회 | - |
dc.contributor.alternativeName | 김경옥 | - |
dc.identifier.bibliographicCitation | 한국해안해양공학회추계학회, pp.72 - 73 | - |
dc.description.journalClass | 2 | - |