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dc.contributor.author塚本, 修ja
dc.contributor.author光田, 寧ja
dc.contributor.alternativeTSUKAMOTO, Osamuen
dc.contributor.alternativeMITSUTA, Yasushien
dc.date.accessioned2009-03-02T07:48:36Z-
dc.date.available2009-03-02T07:48:36Z-
dc.date.issued1983-04-01-
dc.identifier.issn0386-412X-
dc.identifier.urihttp://hdl.handle.net/2433/70553-
dc.description.abstractTurbulence measurements were carried out on the 213m meteorological tower in TsukubaScience City. Water vapor fluctuations were measured together with temperature andthree dimensional wind speed components at 25, 50 and l00m level of the tower. Verticalcoherence of water vapor fluctuations show the form of exponential curve and the decayconstant was evaluated as κ=5. Power spectra of humidity fluctuations and cospectrum ofwater vapor and vertical wind component were obtained. The peak frequency decreaseswith increasing the height of measurement. The variances and covariances of water vaporand vertical wind component also decrease in the upper level. The similarity betweenhumidity and temperature was very good in convective condition for each level.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-
dc.subject.ndc423.84-
dc.title大気境界層における水蒸気変動の乱流特性ja
dc.title.alternativeTURBULENCE CHARACTERISTICS OF WATER VAPOR FLUCTUATION IN THE ATMOSPHERIC BOUNDARY LAYERen
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.volume26-
dc.identifier.issueB-1-
dc.identifier.spage385-
dc.identifier.epage392-
dc.textversionpublisher-
dc.sortkey33-
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:No.26 B-1

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