{"@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/1360011142936021632.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/0022-4073(88)90031-3"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:0022407388900313?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:0022407388900313?httpAccept=text/plain"}}],"dc:title":[{"@value":"Algorithms for radiative intensity calculations in moderately thick atmospheres using a truncation approximation"}],"description":[{"notation":[{"@value":"Abstract   The efficiency of numerical calculations is discussed for selected algorithms employing the discrete ordinate method and the truncation approximation for the solar radiative intensity in moderately thick, plane-parallel scattering atmospheres. It is found that truncation of the phase function causes a significant error in the computed intensity and the magnitude of this error depends significantly on how the intensity is retrieved from the truncated radiative transfer equation. A newly developed retrieval algorithm, the IMS- method, yields the intensity field with an error ⪅1% when the number of discrete path is as small as 10 in the hemisphere for aerosol-laden atmospheres with optical thickness ⪅1."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380011142936021633","@type":"Researcher","foaf:name":[{"@value":"T. Nakajima"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011142936021632","@type":"Researcher","foaf:name":[{"@value":"M. Tanaka"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00224073"}],"prism:publicationName":[{"@value":"Journal of Quantitative Spectroscopy and Radiative Transfer"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"1988-07","prism:volume":"40","prism:number":"1","prism:startingPage":"51","prism:endingPage":"69"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:0022407388900313?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:0022407388900313?httpAccept=text/plain"}],"createdAt":"2003-10-11","modifiedAt":"2019-02-20","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050287297274707328","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Cloud and aerosol contributions to variation in shortwave surface irradiance over East Asia in July during 2001 and 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