{"@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/1390001205221984512.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.2151/sola.2011-044"}},{"identifier":{"@type":"URI","@value":"http://www.jstage.jst.go.jp/article/sola/7/0/7_0_173/_pdf"}},{"identifier":{"@type":"NAID","@value":"130004448551"}}],"dc:title":[{"@language":"en","@value":"Reproducibility of Present Climate in a Non-Hydrostatic Regional Climate Model Nested within an Atmosphere General Circulation Model"}],"dc:language":"en","description":[{"type":"abstract","notation":[{"@language":"en","@value":"A 20-year-integration of a non-hydrostatic regional climate model (NHRCM) was conducted to reproduce the present climate. The annual mean surface temperature and precipitation of Japan are well simulated in NHRCM. There was one conspicuous outlier in the verification of the model's annual precipitation with observations. An even finer grid spacing than 5 km would be required to reproduce the precipitation at this observation point. The regional model successfully simulated heavy precipitation that a general circulation model could not reproduce. This model reproduced snow depth well in most of Japan, except in the north on the coast of the Sea of Japan, where the depth was underestimated."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1410001205221984513","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000257827935"}],"foaf:name":[{"@language":"en","@value":"Sasaki Hidetaka"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Meteorological Research 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Akihiko"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Meteorological Research Institute"}]},{"@id":"https://cir.nii.ac.jp/crid/1410001205221984512","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000257827937"}],"foaf:name":[{"@language":"en","@value":"Hanafusa Mizuki"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Meteorological Research Institute"}]},{"@id":"https://cir.nii.ac.jp/crid/1410001205221984515","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000257827938"}],"foaf:name":[{"@language":"en","@value":"Oh'izumi Mistuo"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Meteorological College"}]},{"@id":"https://cir.nii.ac.jp/crid/1410001205221984514","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000257827939"}],"foaf:name":[{"@language":"en","@value":"Kurihara Kazuo"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Meteorological Research 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EFFECT"},{"@language":"ja","@value":"力学・熱力学効果の観点での降雨の空間偏差要因の分析"}]},{"@id":"https://cir.nii.ac.jp/crid/1390299440019709312","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Global Historical Reanalysis with a 60-km AGCM and Surface Pressure Observations: OCADA"}]},{"@id":"https://cir.nii.ac.jp/crid/1390302459079782144","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Future Projection of Extremely Heavy Rainfall in the Tohoku District of Japan with Large Ensemble Simulations Using the 5 km Regional Climate Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1390565134846897536","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Future Changes of Tropical Cyclones in the Midlatitudes in 4-km-mesh Downscaling Experiments from Large-Ensemble 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