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dc.contributor.author田中, 正昭ja
dc.contributor.alternativeTANAKA, Masaakien
dc.date.accessioned2009-02-10T01:52:09Z-
dc.date.available2009-02-10T01:52:09Z-
dc.date.issued1980-04-01-
dc.identifier.issn0386-412X-
dc.identifier.urihttp://hdl.handle.net/2433/70367-
dc.description.abstractSpecial meteorological observations including the measurements of momentum flux, sensibleheat flux and water vapour flux were carried out, during calm cloudless night, for the study ofthermodynamic behavior of the boundary layer in the case of nocturnal temperature lowing atUjigawa meteorological tower (40 m height) from March 3 to March 4, 1979. Meteorologicalsituations in the lower layer when the temperature cooling occurred in the sorthen part of KyotoBasin were analyzed. Observations were carried out when the radiation fog occurred in thewinter. Themodynamical processes on the formation of radiation fog including the boundaryconditions for the heat flux at the earth surface and the top of fog, and the boundary conditions forthe water vapour flux at the earth surface were discussed on the basis of the observational results.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.ndc451.2-
dc.subject.ndc451.8-
dc.subject.ndc451.62-
dc.title宇治川気象観測塔で観測された冬期の冷えこみと霧についてja
dc.title.alternativeNOCTURNAL TEMPERATURE LOWERING AND FOGS OBSERVED AT UJIGAWA METEOROLOGICAL TOWER IN WINTERen
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.volume23-
dc.identifier.issueB-2-
dc.identifier.spage123-
dc.identifier.epage132-
dc.textversionpublisher-
dc.sortkey09-
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.23 B-2

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