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dc.contributor.author文字, 信貴ja
dc.contributor.author吉門, 洋ja
dc.contributor.author光田, 寧ja
dc.contributor.alternativeMONJI, Nobutakaen
dc.contributor.alternativeYOSHIKADO, Hiroshien
dc.contributor.alternativeMITSUTA, Yasushien
dc.date.accessioned2009-03-02T07:45:06Z-
dc.date.available2009-03-02T07:45:06Z-
dc.date.issued1981-04-01-
dc.identifier.issn0386-412X-
dc.identifier.urihttp://hdl.handle.net/2433/70424-
dc.description.abstractThe temperature, humidity and wind fields of the tropical oceanic boundary layer are investi-gated by lower troposphere radiosondes (LTS). The experiment is a part of the MonsoonExperiment (MONEX) carried out on the R. V. Hakuho-Maru for two weeks in May, 1979.Two different weather situations, I.e., the disturbed and undisturbed periods were chosen toanalyze. The depth of the mixed layer is found to depend on the weather conditions. It developedup to several hundred meters under the undisturbed situations, but reached only a few hundredmeters during the disturbed period. The horizontal wind peak appeared in the stable layer rightabove the mixed layer. The latitudinal variations are also investigated.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.ndc451.24-
dc.subject.ndc451.3-
dc.title熱帯海洋上の大気境界層の構造ja
dc.title.alternativeSTRUCTURE OF THE TROPICAL 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.volume24-
dc.identifier.issueB-1-
dc.identifier.spage371-
dc.identifier.epage380-
dc.textversionpublisher-
dc.sortkey27-
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.24 B-1

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