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dc.contributor.author柿本, 均ja
dc.contributor.author光田, 寧ja
dc.contributor.alternativeKAKIMOTO, Hitoshien
dc.contributor.alternativeMITSUTA, Yasushien
dc.date.accessioned2009-03-02T07:51:09Z-
dc.date.available2009-03-02T07:51:09Z-
dc.date.issued1984-04-01-
dc.identifier.issn0386-412X-
dc.identifier.urihttp://hdl.handle.net/2433/70642-
dc.description.abstractLife cycle of Typhoon 8013 (ORCHID) was analyzed using the infrared brightness data ofthe Geostationary Meteorological Satellite (OMS). This typhoon first appeared as a tropicaldepression near the Caroline Islands Sept. 4, 1980, developed to typhoon intensity a week laternear Okinawa and landed on the southern end of the Kyushu Island. Changes in cloud system areseen prior to the changes in the intensity of the typhoon. The typhoon has shown rapid develop-ment soon after a small dip was seen in the center of a cloud dome top, which means that thetyphoon has changed from one-cell vortex to two-cell vortex. Weakening of the typhoon wasalso seen on the cloud pattern a little before the central pressure increased.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.ndc451.5-
dc.title気象衛星ひまわりの赤外輝度データでみた台風8013(ORCHID)のライフサイクルja
dc.title.alternativeLIFE CYCLE OF TYPHOON 8013 (ORCHID) AS OBSERVED BY THE IR BRIGHTNESS DATA OF GMSen
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.volume27-
dc.identifier.issueB-1-
dc.identifier.spage273-
dc.identifier.epage284-
dc.textversionpublisher-
dc.sortkey24-
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.27 B-1

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