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dc.contributor.author竹見, 哲也ja
dc.contributor.alternativeTAKEMI, Tetsuyaen
dc.date.accessioned2014-02-17T02:01:55Z-
dc.date.available2014-02-17T02:01:55Z-
dc.date.issued2013-09-
dc.identifier.issn0386-412X-
dc.identifier.urihttp://hdl.handle.net/2433/181537-
dc.description.abstractThe severity of meteorological disasters spawned by typhoons critically depends on not only the intensity but also the track of typhoons. A slight change of the track of typhoons would induce a large difference in the intensity and spatial distribution of heavy rainfall and high winds. The present study explores the influences of typhoon tracks on the representations of heavy rainfall and high winds in numerical simulations of typhoon-induced events with the use of a regional meteorological model. The analyses are focused on high-impact typhoons over the Kanto Plain. A nesting capability is used to resolve convective storms embedded in typhoons at the 1-km horizontal grid spacing. A large variability in the representations of heavy rainfall and high winds is demonstrated.en
dc.format.mimetypeapplication/pdf-
dc.language.isojpn-
dc.publisher京都大学防災研究所ja
dc.publisher.alternativeDisaster Prevention Research Institute, Kyoto Universityen
dc.subject台風ja
dc.subject台風経路ja
dc.subject風水害ja
dc.subject気象モデルja
dc.subjecttyphoonen
dc.subjecttyphoon tracken
dc.subjecttyphoon disasteren
dc.subjectmeteorological modelen
dc.subject.ndc519.9-
dc.title台風経路の違いによる風水害への影響についてja
dc.title.alternativeInfluences of Typhoon Tracks on the Severity of Rain and Wind Stormsen
dc.typedepartmental bulletin paper-
dc.type.niitypeDepartmental Bulletin Paper-
dc.identifier.ncidAN00027784-
dc.identifier.jtitle京都大学防災研究所年報. Bja
dc.identifier.volume56-
dc.identifier.issueB-
dc.identifier.spage285-
dc.identifier.epage290-
dc.textversionpublisher-
dc.sortkey34-
dc.relation.urlhttp://www.dpri.kyoto-u.ac.jp/nenpo/nenpo.html-
dcterms.accessRightsopen access-
dc.identifier.pissn0386-412X-
dc.identifier.jtitle-alternativeDisaster Prevention Research Institute Annuals. Ben
出現コレクション:Vol.56 B

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