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dc.contributor.author向川, 均ja
dc.contributor.author野口, 峻佑ja
dc.contributor.author黒田, 友二ja
dc.contributor.author水田, 亮ja
dc.contributor.author小寺, 邦彦ja
dc.contributor.alternativeMUKOUGAWA, Hitoshien
dc.contributor.alternativeNOGUCHI, Shunsukeen
dc.contributor.alternativeKURODA, Yuhjien
dc.contributor.alternativeMIZUTA, Ryoen
dc.contributor.alternativeKODERA, Kunihikoen
dc.contributor.transcriptionムコウガワ, ヒトシja-Kana
dc.contributor.transcriptionノグチ, シュンスケja-Kana
dc.contributor.transcriptionクロダ, ユウジja-Kana
dc.contributor.transcriptionミズタ, リョウja-Kana
dc.contributor.transcriptionコデラ, クニヒコja-Kana
dc.date.accessioned2018-12-25T23:39:22Z-
dc.date.available2018-12-25T23:39:22Z-
dc.date.issued2018-09-
dc.identifier.issn0386-412X-
dc.identifier.urihttp://hdl.handle.net/2433/235855-
dc.description.abstractThe predictability of two stratospheric sudden warming (SSW) events occurring in 2009 and 2010 is examined by conducting ensemble forecast using an AGCM. It is found that the predictable period of the vortex splitting SSW in 2009 is about 7 days, much shorter than that of the vortex-displacement SSW in 2010, which is assessed at about 14 days. Stability analysis of the stratospheric circulation using a nondivergent barotropic vorticity equation also reveals that the upper stratospheric circulation is highly unstable to infinitesimal perturbations just before the mature phase of the 2009 SSW event while such unstable modes with extremely large growth rates are absent during the 2010 SSW event. Hence, it is suggested that a predictability barrier inherent in the upper stratospheric circulation, which is characterized by the existence of dynamically unstable modes with large growth rates limits a predictable period of the 2009 SSW event.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成層圏突然昇温ja
dc.subject予測可能性ja
dc.subject力学的安定性ja
dc.subjectstratospheric sudden warmingen
dc.subjectpredictabilityen
dc.subjectdynamical stabilityen
dc.subject.ndc519.9-
dc.title冬季成層圏極渦に内在する予測障壁 --2009・2010年の成層圏突然昇温の予測可能性比較--ja
dc.title.alternativeOn the Existence of the Predictability Barrier in the Wintertime Stratospheric Polar Vortex: Intercomparison on the Predictability of the Two Stratospheric Sudden Warmings in 2009 and 2010en
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.volume61-
dc.identifier.issueB-
dc.identifier.spage360-
dc.identifier.epage365-
dc.textversionpublisher-
dc.sortkey16-
dc.address京都大学大学院理学研究科ja
dc.address気象研究所気候研究部ja
dc.address気象大学校ja
dc.address気象研究所気候研究部ja
dc.address気象研究所気候研究部ja
dc.address.alternativeGraduate School of Science, Kyoto Universityen
dc.address.alternativeClimate Research Department, Meteorological Research Instituteen
dc.address.alternativeMeteorological Collegeen
dc.address.alternativeClimate Research Department, Meteorological Research Instituteen
dc.address.alternativeClimate Research Department, Meteorological Research Instituteen
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.61 B

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