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dc.contributor.author堀口, 光章ja
dc.contributor.alternativeHORIGUCHI, Mitsuakien
dc.date.accessioned2023-02-21T09:31:38Z-
dc.date.available2023-02-21T09:31:38Z-
dc.date.issued2022-12-
dc.identifier.urihttp://hdl.handle.net/2433/279423-
dc.description.abstractWind speed in the atmospheric boundary layer (ABL) changes in a variety of time scales. During autumn season, stability of the ABL varies from near neutral to unstable conditions in the daytime. This certainly affects the wind near the surface. In this study, variation of the wind at two places was investigated. At the Ujigawa Open Laboratory in Kyoto City, intermittent events of large fluxes in the surface layer were observed by sonic anemometers at around midday and in the afternoon. On the other hand, at the Nagoya Local Meteorological Observatory in Nagoya City, a wind profiler shows that the difference of wind speeds at the observation levels becomes small in the morning and the wind speeds gradually increase in the afternoon.en
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大気境界層ja
dc.subject風速変動ja
dc.subject乱流輸送ja
dc.subject超音波風速計ja
dc.subjectウィンドプロファイラja
dc.subjectatmospheric boundary layeren
dc.subjectwind variationen
dc.subjectturbulent transferen
dc.subjectsonic anemometeren
dc.subjectwind profileren
dc.subject.ndc519.9-
dc.title秋季における大気境界層での風速変動ja
dc.title.alternativeWind Variation in the Atmospheric Boundary Layer during Autumn Seasonen
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.volume65-
dc.identifier.issueB-
dc.identifier.spage134-
dc.identifier.epage145-
dc.textversionpublisher-
dc.sortkey13-
dc.address京都大学防災研究所ja
dc.relation.urlhttp://www.dpri.kyoto-u.ac.jp/publications/nenpo/-
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.65 B

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