{"@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/1390282681480247424.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.2151/jmsj.84.691"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"8027813"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/bib/8027813"}},{"identifier":{"@type":"URI","@value":"https://ndlsearch.ndl.go.jp/books/R000000004-I8027813"}},{"identifier":{"@type":"URI","@value":"https://dl.ndl.go.jp/pid/10612693"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"10612693"}},{"identifier":{"@type":"NAID","@value":"110004804530"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/digimeta/10612693"}},{"identifier":{"@type":"URI","@value":"http://www.jstage.jst.go.jp/article/jmsj/84/4/84_4_691/_pdf"}},{"identifier":{"@type":"URI","@value":"http://dl.ndl.go.jp/info:ndljp/pid/10612693"}}],"dc:title":[{"@language":"en","@value":"Radiative Effects on Precipitation: A South China Storm Case Study"}],"dc:language":"en","description":[{"type":"abstract","notation":[{"@language":"en","@value":"In this paper the effects of radiation on a meso-scale precipitating system is investigated during a severe storm in South China on June 8, 1998. This was done by using the Pennsylvania State University (PSU)/National Center for Atmospheric Research (NCAR)/Meso-scale Model 5 Version 3 (MM5_V3) after the introduction of radiative transfer schemes that are able to treat water clouds, ice crystals, snow, and groupel. The results suggest that the rainfall patterns do not differ too much for the various radiation schemes used in the numerical calculations, but rather influence the rainfall intensity in the central areas. The radiative effects on precipitation are more significant during daytime, as compared to nighttime. The diurnal variation of rainfall is enhanced by the radiative processes. Computed precipitation intensities, and radiative cooling/heating rates, are dependent on the specific radiative transfer scheme used. The results suggest that model improvement of daytime cloud radiative processes is crucial for a better representation of such effects on meso-scale precipitating system."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1410282681480247425","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000363502907"}],"foaf:name":[{"@language":"en","@value":"ZHOU Guanqiang"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Shanghai Typhoon Institute/Chinese Meteorological Administration, Shanghai"},{"@language":"en","@value":"Department of Atmospheric Science, School of Physics, Peking University, Beijing"}]},{"@id":"https://cir.nii.ac.jp/crid/1410282681480247424","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000363502296"}],"foaf:name":[{"@language":"en","@value":"ZHAO Chunsheng"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Department of Atmospheric Science, School of Physics, Peking University, Beijing"}]},{"@id":"https://cir.nii.ac.jp/crid/1410282681480247427","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000363502909"}],"foaf:name":[{"@language":"en","@value":"DUAN Ying"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Hebei Meteorological Bureau"}]},{"@id":"https://cir.nii.ac.jp/crid/1410282681480247426","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000363502910"}],"foaf:name":[{"@language":"en","@value":"QIN Yu"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Department of Atmospheric Science, School of Physics, Peking University, Beijing"}]}],"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. 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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":"2006","prism:volume":"84","prism:number":"4","prism:startingPage":"691","prism:endingPage":"704"},"reviewed":"false","url":[{"@id":"http://id.ndl.go.jp/bib/8027813"},{"@id":"https://ndlsearch.ndl.go.jp/books/R000000004-I8027813"},{"@id":"https://dl.ndl.go.jp/pid/10612693"},{"@id":"http://id.ndl.go.jp/digimeta/10612693"},{"@id":"http://www.jstage.jst.go.jp/article/jmsj/84/4/84_4_691/_pdf"},{"@id":"http://dl.ndl.go.jp/info:ndljp/pid/10612693"}],"availableAt":"2006","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360011142932313728","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Diurnal Variation of Deep Cumulus Convection"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142938142336","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Numerical Study of Convection Observed during the Winter Monsoon Experiment Using a Mesoscale Two-Dimensional Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292618895560320","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"On the Computation of Saturation Vapor Pressure"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292620825307136","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Parameterization of the Radiative Properties of Cirrus Clouds"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574093637712384","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Heating Rates in Tropical Anvils"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567863258880","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"On the Correlated<i>k</i>-Distribution Method for Radiative Transfer in Nonhomogeneous Atmospheres"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567867167488","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Radiative transfer for inhomogeneous atmospheres: RRTM, a validated correlated‐k model for the longwave"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855568987953536","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Delta-Eddington Approximation for Radiative Flux Transfer"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855569070396416","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Numerical Simulations of a Heavy Rainfall Case in South China"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855571171020416","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Actinic Flux and Net Flux Calculations in Radiative Transfer—A Comparative Study of Computational Efficiency"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855571495572224","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Impact of the Ice Phase and Radiation on a Midlatitude Squall Line System"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418518664611584","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A new convective adjustment scheme. 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