{"@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/1390001205290977792.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.3178/hrl.4.6"}},{"identifier":{"@type":"NAID","@value":"130000248959"}}],"dc:title":[{"@language":"en","@value":"Statistical analysis of simulated direct and indirect precipitation associated with typhoons around Japan using a cloud-system resolving model"}],"dc:language":"en","description":[{"type":"abstract","notation":[{"@language":"en","@value":"To validate the reproducibility of simulated typhoons and related precipitation, perfect boundary condition experiments, forced by 20-km-mesh Japan Meteorological Agency (JMA) operational regional objective analysis (RANAL) data from June to October in 2002-2006, are performed using a 5-km-mesh cloud-system resolving nonhydrostatic regional climate model (NHM-5km). <br>NHM-5km reproduced all 57 typhoons observed in the model domain during the experiment period. Relative to JMA best track data for the typhoons, the average position error of typhoon centers is 130 km at 72 hours after typhoon genesis or when the typhoon first enters the model domain. The simulated minimum central pressures of typhoons are similar to those in RANAL data. The precipitation within (outside of) a 300-km radius from the center of each typhoon is defined as direct (indirect) precipitation. The distributions of the simulated direct and indirect precipitation of typhoons show good agreement with precipitation analyses by JMA. For hourly precipitation amounts exceeding 5 mm, direct precipitation is observed more frequently than is indirect precipitation, especially for amounts exceeding 20 mm. These features are well reproduced by NHM-5km. The appearance frequency of simulated direct precipitation for hourly precipitation amounts also shows a good quantitative agreement with that measured by raingauges."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420001326232041088","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"40713954"},{"@type":"NRID","@value":"1000040713954"},{"@type":"ORCID","@value":"0000-0003-3839-3826"},{"@type":"NRID","@value":"9000001341720"},{"@type":"NRID","@value":"9000020296335"},{"@type":"NRID","@value":"9000283593635"},{"@type":"NRID","@value":"9000257827581"},{"@type":"NRID","@value":"9000415323859"},{"@type":"NRID","@value":"9000257768330"},{"@type":"NRID","@value":"9000021862011"},{"@type":"NRID","@value":"9000020230447"},{"@type":"NRID","@value":"9000018916419"},{"@type":"NRID","@value":"9000402246598"},{"@type":"NRID","@value":"9000257768313"},{"@type":"NRID","@value":"9000257768247"},{"@type":"NRID","@value":"9000370744987"},{"@type":"NRID","@value":"9000018916424"},{"@type":"NRID","@value":"9000370254208"},{"@type":"NRID","@value":"9000020194446"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/masuo"}],"foaf:name":[{"@language":"en","@value":"Nakano Masuo"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Advanced Earth Science and Technology Organization"}]},{"@id":"https://cir.nii.ac.jp/crid/1410001205290977793","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000020296341"}],"foaf:name":[{"@language":"en","@value":"Kanada Sachie"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Advanced Earth Science and Technology Organization"}]},{"@id":"https://cir.nii.ac.jp/crid/1410001205290977792","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000020296348"}],"foaf:name":[{"@language":"en","@value":"Kato Teruyuki"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Meteorological Research Institute"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"18823416"},{"@type":"LISSN","@value":"18823416"}],"prism:publicationName":[{"@language":"en","@value":"Hydrological Research Letters"},{"@language":"en","@value":"Hydrological Research Letters"}],"dc:publisher":[{"@language":"en","@value":"Japan Society of Hydrology and Water Resources (JSHWR) / Japanese Association of Groundwater Hydrology (JAGH) / Japanese Association of Hydrological Sciences (JAHS) / Japanese Society of Physical Hydrology (JSPH)"},{"@language":"ja","@value":"水文・水資源学会／日本地下水学会／日本水文科学会／陸水物理研究会"}],"prism:publicationDate":"2010","prism:volume":"4","prism:startingPage":"6","prism:endingPage":"10"},"reviewed":"false","availableAt":"2010","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050282810812286080","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Impact assessment of coastal hazards due to future changes of tropical cyclones in the North Pacific Ocean"},{"@value":"Impact assessment of coastal hazards due to future changes in tropical cyclones in the North Pacific Ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292621137009024","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A One-Dimensional Entraining/Detraining Plume Model and Its Application in Convective Parameterization"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092889948288","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Role of Typhoon Songda (2004) in Producing Distantly Located Heavy Rainfall in Japan*"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894977543680","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Performance of Long-Term Integrations of the Japan Meteorological Agency Nonhydrostatic Model Using the Spectral Boundary Coupling Method"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388845119130240","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Validation of present-day regional climate simulations over Europe: LAM simulations with observed boundary conditions"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205289671168","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Projection of changes in future weather extremes using super-high-resolution global and regional atmospheric models in the KAKUSHIN Program: Results of preliminary experiments"},{"@value":"Projection of changes in future weather extremes using super-high-resolution global and regional atmospheric models in the KAKUSHIN program"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206503268352","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Dynamical Downscaling for Climate Projection with High-Resolution MRI AGCM-RCM"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206504122752","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"孤立した対流雲の力学的•微物理学的変化の数値モデリング"},{"@language":"en","@value":"Numerical Modeling of Dynamical and Microphysical Evolution of an Isolated Convective Cloud"},{"@value":"Numerical modeling of dynamical and microphysical evolution of an isolated convective cloud—The 19 July 1981 CCOPE cloud"},{"@value":"Numerical modeling of dynamical and microphysical evolution of an isolated convective cloud: the 19 July 1981 CCOPE cloud"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206504722816","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tropical Cyclone Climatology in a Global-Warming Climate as Simulated in a 20 km-Mesh Global Atmospheric Model: Frequency and Wind Intensity Analyses"},{"@value":"Tropical cyclone climatology in a global warming climate as simulated in a 20-km-mesh global atmospheric model: frequency and wind intensity analysis"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001277391245440","@type":"Article","resourceType":"学術雑誌論文(journal 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Century Projected by a High-Resolution Regional Climate Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681480066816","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Nonhydrostatic Atmospheric Models and Operational Development at JMA"},{"@value":"Nonhydrostatic Atmospheric Models and Operational Development at JMA(125th Anniversary Issue of the Meteorological Society of Japan)"},{"@value":"Nonhydrostatic atmosperic models and operational development at JMA"},{"@value":"Nonhydrostatic atmospheric models operational development at JMA"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681480967680","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"20-km-Mesh Global Climate Simulations Using JMA-GSM Model<br>—Mean Climate States—"},{"@value":"20-km-Mesh Global Climate Simulations Using JMA-GSM Model--Mean Climate States"},{"@value":"20-km-Mesh Global Climate Simulations Using JMA-GSM 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ケンキュウ シュウカイ ヨリ ヨイ ショウライ ヨソク オ メザシテ"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892096588672","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Scalability of future climate changes across Japan examined with large-ensemble simulations at +1.5K, +2K, and +4K global warming 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