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dc.contributor.author鵜沼, 昂ja
dc.contributor.author竹見, 哲也ja
dc.contributor.alternativeUNUMA, Takashien
dc.contributor.alternativeTAKEMI, Tetsuyaen
dc.date.accessioned2016-04-07T02:40:54Z-
dc.date.available2016-04-07T02:40:54Z-
dc.date.issued2015-06-
dc.identifier.issn0386-412X-
dc.identifier.urihttp://hdl.handle.net/2433/210076-
dc.description.abstractRole of middle-level moisture on the development of quasi-stationary convective systems (QSCSs) in humid environments was investigated using a numerical cloud model in an idealized framework. As moisture increased at the middle levels, the static stability in the low-to-middle troposphere was decreased due to preceding deep convections. Trajectory analysis indicated that the parcels were able to go upward by experiencing positive buoyancy when the environmental moisture in the middle troposphere is large. Therefore, it is suggested that the development of QSCSs in humid environments is explained by positive buoyancy that is induced by the larger environmental moisture.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停滞性降水系ja
dc.subject中・下層水蒸気量ja
dc.subjectメソ気象学ja
dc.subjectquasi-stationary convective systemen
dc.subjectlow-to-middle level moistureen
dc.subjectmesoscale meteorologyen
dc.subject.ndc519.9-
dc.title湿潤な環境下で発生する停滞性降水系の理想化数値実験ja
dc.title.alternativeNumerical Experiments of Quasi-Stationary Mesoscale Convective Systems in Humid Environmentsen
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.volume58-
dc.identifier.issueB-
dc.identifier.spage167-
dc.identifier.epage174-
dc.textversionpublisher-
dc.sortkey22-
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.58 B

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