{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1360004236560264704.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1175/mwr-d-18-0457.1"}},{"identifier":{"@type":"URI","@value":"http://journals.ametsoc.org/mwr/article-pdf/147/5/1557/4862283/mwr-d-18-0457_1.pdf"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"The Relationship between Convective Bursts and Warm-Core Intensification in a Nonhydrostatic Simulation of Typhoon Lionrock (2016)"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title>\n               <jats:p>Typhoon Lionrock (2016) was unusual among tropical cyclones (TCs) in that it formed east of the monsoon gyre in the western North Pacific, and moved counterclockwise. It rapidly intensified in the monsoon gyre in an environment of weak upper-tropospheric winds and vertical wind shear. This study used a 3-km mesh nonhydrostatic model to examine the warm-core intensification of Typhoon Lionrock, which was associated with cyclone-scale vigorous convection [i.e., convective bursts (CBs)]. The simulation reproduced the multiple CBs at intervals of 1 day or shorter, which were related to the diurnal cycles and other short time-scale variations in the TC convection. Each CB tended to precede peak temperature anomalies near the TC center by 0–12 h, indicating that the warm-core intensification occurred due to diabatic heating released by the vigorous eyewall convection. Notably, updrafts due to convection during the intensification phase were stronger than those occurring during the mature and decay phases, and the maximum temperature anomaly of the upper-tropospheric warm core rapidly increased during eyewall formation. In addition, this study indicated that most of the asymmetric inner-core vigorous convection associated with CBs, which was induced by the vertical wind shear, contributed to the warm-core intensification. Furthermore, the budget analysis of potential temperature within the TC inner core showed that adiabatic heating due to subsidence from near the tropopause within the eye, often following CBs, was essential in developing the eye. The lag correlation suggested the lag time between the CBs and the subsidence within the eye was 3–9 h.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004236560264705","@type":"Researcher","foaf:name":[{"@value":"Ryo Oyama"}],"jpcoar:affiliationName":[{"@value":"Meteorological Research Institute, Japan Meteorological Agency, Tsukuba, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1420564276160601216","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"20354475"},{"@type":"NRID","@value":"1000020354475"},{"@type":"CINII_AUTHOR_ID","@value":"DA18490340"},{"@type":"URI","@value":"https://ci.nii.ac.jp/author/DA18490340#entity"},{"@type":"URI","@value":"https://viaf.org/viaf/NII%7CDA18490340"},{"@type":"NRID","@value":"9000001423497"},{"@type":"NRID","@value":"9000363486421"},{"@type":"NRID","@value":"9000402818771"},{"@type":"NRID","@value":"9000001026251"},{"@type":"NRID","@value":"9000253191152"},{"@type":"NRID","@value":"9000409504836"},{"@type":"NRID","@value":"9000301746333"},{"@type":"NRID","@value":"9000399261804"},{"@type":"NRID","@value":"9000415409155"},{"@type":"NRID","@value":"9000391637149"},{"@type":"NRID","@value":"9000356661487"},{"@type":"NRID","@value":"9000409895918"},{"@type":"NRID","@value":"9000241203935"},{"@type":"NRID","@value":"9000257827841"},{"@type":"NRID","@value":"9000410889306"},{"@type":"NRID","@value":"9000379602814"},{"@type":"NRID","@value":"9000324997413"},{"@type":"NRID","@value":"9000315141630"},{"@type":"NRID","@value":"9000414745635"},{"@type":"NRID","@value":"9000398988828"},{"@type":"NRID","@value":"9000257979045"},{"@type":"NRID","@value":"9000257978984"},{"@type":"NRID","@value":"9000404156868"},{"@type":"NRID","@value":"9000411827868"},{"@type":"NRID","@value":"9000008080117"},{"@type":"NRID","@value":"9000414742080"},{"@type":"NRID","@value":"9000404149326"},{"@type":"NRID","@value":"9000356661375"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/Typhoon"}],"foaf:name":[{"@value":"Akiyoshi Wada"}],"jpcoar:affiliationName":[{"@value":"Meteorological Research Institute, Japan Meteorological Agency, Tsukuba, Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00270644"},{"@type":"EISSN","@value":"15200493"}],"prism:publicationName":[{"@value":"Monthly Weather Review"}],"dc:publisher":[{"@value":"American Meteorological Society"}],"prism:publicationDate":"2019-04-17","prism:volume":"147","prism:number":"5","prism:startingPage":"1557","prism:endingPage":"1579"},"reviewed":"false","dc:rights":["http://www.ametsoc.org/PUBSReuseLicenses"],"url":[{"@id":"http://journals.ametsoc.org/mwr/article-pdf/147/5/1557/4862283/mwr-d-18-0457_1.pdf"}],"createdAt":"2019-02-28","modifiedAt":"2020-12-07","project":[{"@id":"https://cir.nii.ac.jp/crid/1040000781844938112","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"15K05292"},{"@type":"JGN","@value":"JP15K05292"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-15K05292/"}],"notation":[{"@language":"ja","@value":"台風強度予測精度向上のための台風強化停止プロセスの解明"},{"@language":"en","@value":"Clarification of cessation mechanisms of tropical cyclone intensification for developing tropical cyclone intensity forecasts"}]},{"@id":"https://cir.nii.ac.jp/crid/1040000781998319488","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"18K03747"},{"@type":"JGN","@value":"JP18K03747"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-18K03747/"}],"notation":[{"@language":"ja","@value":"新世代気象衛星のマルチバンド観測を用いた台風の暖気核発達プロセスの解明"},{"@language":"en","@value":"Elucidation of tropical cyclone warm core development processes using multi-band observations by new generation satellites"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360011142932316928","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"On the Development of Double Warm-Core Structures in Intense Tropical Cyclones"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142933475584","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Meteorological Research Institute multivariate ocean variational estimation (MOVE) system: Some early 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article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The Diurnal Cycle of Clouds in Tropical Cyclones over the Western North Pacific Basin"}]},{"@id":"https://cir.nii.ac.jp/crid/1390010292913761664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Interactions between a Tropical Cyclone and Upper-Tropospheric Cold-Core Lows Simulated by an Atmosphere-Wave-Ocean Coupled Model: A Case Study of Typhoon Jongdari (2018)"},{"@language":"ja","@value":"大気波浪海洋結合モデルでシミュレーションされた熱帯低気圧と対流圏上層寒冷低気圧相互作用：2018年台風ジョンダリの事例解析"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681434113920","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Estimation of tropical cyclone central pressure from warm core intensity observed by the Advanced Microwave Sounding Unit-A (AMSU-A)"},{"@language":"ja","@value":"改良型マイクロ波探査計（AMSU-A）で観測される暖気核の強さを用いた熱帯低気圧の中心気圧の推定"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681477408256","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Periodic Time Variation of a Low-TBB Cloud Area in Typhoon"},{"@value":"Periodic time variation of low-TBB cloud area in typhoon"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681480300288","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"TBB分布及び眼径に現われた台風の日変化"},{"@language":"en","@value":"Diurnal Variations of Satellite-Measured TBB Areal Distribution and Eye Diameter of Mature Typhoons"},{"@value":"Radiative forcing of simulated tropical cloud clusters"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681483058560","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Diagnosis of Tropical Cyclone Intensity and Structure Using Upper Tropospheric 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