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No convective clouds were observed near its center, nor did typical cloud patterns with spiral bands and eyewalls appear in the storm. Reanalysis data (ERA-Interim) was used in this study, and a set of sensitivity experiments conducted with a numerical model (NICAM) to examine the cause of the explosive convection.<br> The analyses of the reanalysis data elucidated mechanisms for excitation of deep convection, including a high convective available potential energy environment due to moisture convergence at lower levels, potential vorticity generation by a diabatic Rossby vortex mechanism, and dynamical forcing formation of upward motion induced by upper levels.<br> Moreover, two sensitivity experiments were conducted by modifying the vortex structure of Bebinca. The results suggested that Bebinca’s unusual characteristic, the weak low-level pressure gradient near the center was fundamental for excitation of the explosive convection in the northern area."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1410282681482232192","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000257768755"}],"foaf:name":[{"@language":"en","@value":"ARAKANE Sho"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Atmosphere and Ocean Research Institute, The University of Tokyo, Kashiwa, 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Wataru"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Atmosphere and Ocean Research Institute, The University of Tokyo, Kashiwa, Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00261165"},{"@type":"LISSN","@value":"00261165"},{"@type":"EISSN","@value":"21869057"},{"@type":"NDL_BIB_ID","@value":"000000388871"},{"@type":"ISSN","@value":"00261165"},{"@type":"NCID","@value":"AA00702524"}],"prism:publicationName":[{"@language":"ja","@value":"気象集誌. 第2輯"},{"@value":"気象集誌. 第2輯"},{"@language":"en","@value":"Journal of the Meteorological Society of Japan. Ser. II"},{"@language":"ja","@value":"気象集誌"},{"@language":"ja","@value":"氣象集誌. 第2輯"},{"@language":"en","@value":"Journal of the Meteorological Society of Japan"},{"@language":"en","@value":"JMSJ"}],"dc:publisher":[{"@language":"en","@value":"Meteorological Society of Japan"},{"@language":"ja","@value":"公益社団法人 日本気象学会"}],"prism:publicationDate":"2014","prism:volume":"92","prism:number":"2","prism:startingPage":"141","prism:endingPage":"161"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"http://id.ndl.go.jp/bib/025417286"},{"@id":"https://ndlsearch.ndl.go.jp/books/R000000004-I025417286"},{"@id":"https://www.jstage.jst.go.jp/article/jmsj/92/2/92_2014-201/_pdf"}],"availableAt":"2014","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=tropical%20cyclone","dc:title":"tropical cyclone"},{"@id":"https://cir.nii.ac.jp/all?q=extratropical%20transition","dc:title":"extratropical transition"},{"@id":"https://cir.nii.ac.jp/all?q=diabatic%20Rossby%20vortex","dc:title":"diabatic Rossby vortex"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040000782182449408","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"23740349"},{"@type":"JGN","@value":"JP23740349"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-23740349/"}],"notation":[{"@language":"ja","@value":"低気圧の多様性に関する高解像領域モデルによる理想化実験"},{"@language":"en","@value":"Idealized experiments on diversity of cyclones using a high-resolution regional model."}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050564285797115264","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Application of a global nonhydrostatic model with a stretched-grid system to regional aerosol simulations around Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142933994112","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Madden-Julian Oscillation Event Realistically Simulated by a Global Cloud-Resolving Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142935298688","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A new dynamical framework of nonhydrostatic global model using the icosahedral grid"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142937337216","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Response of Balanced Hurricanes to Local Sources of Heat and Momentum"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142940931072","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A k-distribution-based radiation code and its computational optimization for an atmospheric general circulation model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145885130752","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Asian summer monsoon simulated by a global cloud‐system‐resolving model: Diurnal to intra‐seasonal variability"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617911043328","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The ERA‐Interim reanalysis: configuration and performance of the data assimilation system"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619301317888","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Extratropical Transition of Southwest Pacific Tropical Cyclones. 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