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dc.contributor.author山元, 龍三郎ja
dc.contributor.author岩嶋, 樹也ja
dc.contributor.author星合, 誠ja
dc.contributor.alternativeYAMAMOTO, Ryozaburoen
dc.contributor.alternativeIWASHIMA, Tatsuyaen
dc.contributor.alternativeHOSHIAI, Makotoen
dc.date.accessioned2009-01-30T05:00:09Z-
dc.date.available2009-01-30T05:00:09Z-
dc.date.issued1973-04-01-
dc.identifier.issn0386-412X-
dc.identifier.urihttp://hdl.handle.net/2433/69879-
dc.description.abstractDaily behaviours of the quasi-stationary part and travelling one of the ultra-long waves areanalyzed at 300 mb in the latitudinal zone from 300 N to 850 N for period of February-March 1968, in which a significant blocking action occurs in the North Atlantic. Remarkable amplificationof the quasi-stationary waves of wavenumbers 1 and 4, the phases of which agree approximatelywith the location of the blocking high, is noticed during the period of the blocking action. Cor-responding to this amplification, the amplitudes of travelling waves of wavenumbers 1 and 3 and ofthe quasi-stationary waves of wavenuinbers 2 and 3 decrease. This fact suggests that exchange ofthe energy may take place between travelling wave and quasi-stationary one of each wavenumber.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.ndc451.3-
dc.subject.ndc451.85-
dc.title大気大循環の変動と異常気象(III)ja
dc.title.alternativeFLUCTUATIONS OF THE ATMOSPHERIC GENERAL CIRCULATION AND ABNORMAL WEATHER (III)en
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.volume16-
dc.identifier.issueB-
dc.identifier.spage343-
dc.identifier.epage360-
dc.textversionpublisher-
dc.sortkey29-
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.16 B

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