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dc.contributor.author光田, 寧ja
dc.contributor.alternativeMITSUTA, Yasushien
dc.date.accessioned2009-01-29T05:03:49Z-
dc.date.available2009-01-29T05:03:49Z-
dc.date.issued1964-03-01-
dc.identifier.issn0386-412X-
dc.identifier.urihttp://hdl.handle.net/2433/69174-
dc.description.abstractThree dimensional wind components at 1Gm from the ground in typhoon winds are studiedby the use of a propeller anemometer and the new all-weather type bivane, whose free periodis about 15/V sec and damping ratio is 0.15, at Shionomisaki Wind Observatory of Kyoto Univ.The data used in this study was odtained on Aug. 2~, 1963 when typhoon 6311 was passingover the southern ocean of Shionomisaki. The mean wind speed over the sampling duration(6 mm) was 18.3 in/sec. The vertical fluctuating components are smaller than longitudinal ones, and decrease more rapidly with averaging time than those. The ratio is about 20-'3l~%for a few seconds averaged wind speed, but it becomes nearly 10% for 20 or 30sec. Andthe correlation coefficient between longitudinal and vertical components is about 07.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.ndc451.5-
dc.title暴風時における風速の垂直成分についてja
dc.title.alternativeVERTICAL GUSTS NEAR SURFACE IN HIGH WINDSen
dc.typedepartmental bulletin paper-
dc.type.niitypeDepartmental Bulletin Paper-
dc.identifier.ncidAN10334870-
dc.identifier.jtitle京都大学防災研究所年報ja
dc.identifier.volume7-
dc.identifier.spage199-
dc.identifier.epage206-
dc.textversionpublisher-
dc.sortkey17-
dc.relation.urlhttp://www.dpri.kyoto-u.ac.jp/nenpo/nenpo.html-
dcterms.accessRightsopen access-
dc.identifier.jtitle-alternativeDisaster Prevention Research Institute Annualsen
出現コレクション:No.7

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