{"@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/1362262946068249728.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.atmosenv.2011.03.037"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S1352231011002974?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S1352231011002974?httpAccept=text/plain"}}],"dc:title":[{"@value":"Global aerosol model-derived black carbon concentration and single scattering albedo over Indian region and its comparison with ground observations"}],"description":[{"notation":[{"@value":"Abstract   Black carbon (BC) aerosols through their light-absorbing properties create strong perturbation in the atmosphere by heating the atmosphere. BC mass concentration and single scattering albedo (SSA) are important parameters to investigate atmospheric heating. In the present study, measurements of BC and SSA over Indian region from the literature are summarized and compared with simulations by a global aerosol model SPRINTARS. It has been observed that BC emission inventory widely used in the world is underestimating and the model simulated SSA tends to be higher than observed-SSA. In addition to the inventory, we have run the global model using the different BC emission inventory interpolated by  Streets et al. (2003)  over Asia. The model runs with this inventory was found to provide comparable results with ground observations for BC and SSA. Aerosol radiative forcing due to direct effect (ADRF) over Indian region estimated to be −2.76 W m −2  at the surface and −1.91 W m −2  at the atmosphere using the modified emission inventory in the global aerosol model. The atmospheric heating is estimated to be +0.85 W m −2 , which is three times higher than the original emission inventory estimated value of +0.25 W m −2 . Results of the study suggest that the differences in various BC emission inventories widely used in the world’s research community should be studied for proper estimation of the aerosol radiative forcing over the Indian region."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004230585751810","@type":"Researcher","foaf:name":[{"@value":"D. Goto"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262946068249728","@type":"Researcher","foaf:name":[{"@value":"T. Takemura"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262946068249730","@type":"Researcher","foaf:name":[{"@value":"T. Nakajima"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262946068249729","@type":"Researcher","foaf:name":[{"@value":"K.V.S. Badarinath"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"13522310"}],"prism:publicationName":[{"@value":"Atmospheric Environment"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2011-06","prism:volume":"45","prism:number":"19","prism:startingPage":"3277","prism:endingPage":"3285"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/","https://www.elsevier.com/legal/tdmrep-license","http://www.elsevier.com/open-access/userlicense/1.0/","https://doi.org/10.15223/policy-017","https://doi.org/10.15223/policy-037","https://doi.org/10.15223/policy-012","https://doi.org/10.15223/policy-029","https://doi.org/10.15223/policy-004"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S1352231011002974?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S1352231011002974?httpAccept=text/plain"}],"createdAt":"2011-04-14","modifiedAt":"2025-10-22","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Atmospheric%20Science","dc:title":"Atmospheric Science"},{"@id":"https://cir.nii.ac.jp/all?q=Environmental%20Science(all)","dc:title":"Environmental Science(all)"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050564285797115264","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Application of a global nonhydrostatic model with a stretched-grid system to regional aerosol simulations around Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004230585752064","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Multi-scale Simulations of Atmospheric Pollutants Using a Non-hydrostatic Icosahedral Atmospheric Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004231220404736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Synoptic weather conditions and aerosol episodes over Indo-Gangetic Plains, India"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233292788352","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Hourly Aerosol Assimilation of Himawari‐8 AOT Using the Four‐Dimensional Local Ensemble Transform Kalman Filter"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004240186417536","@type":"Article","resourceType":"preprint","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Impact of the aging process of black carbon aerosols on their spatial distribution, hygroscopicity, and radiative forcing in a global climate model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182086147200","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Modeling of black carbon in Asia using a global-to-regional seamless aerosol-transport model"}]},{"@id":"https://cir.nii.ac.jp/crid/2050870367073300736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A development of reduction scenarios of the short-lived climate pollutants (SLCPs) for mitigating global warming and environmental problems"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842089639168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The Non-hydrostatic Icosahedral Atmospheric Model : description and development"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/j.atmosenv.2011.03.037"},{"@type":"OPENAIRE","@value":"doi_dedup___::1665d8fb2f638706016f913b98637913"},{"@type":"CROSSREF","@value":"10.5194/gmd-8-235-2015_references_DOI_D9OVbaNZjyMzJSWnVhOYDK6wJEN"},{"@type":"CROSSREF","@value":"10.1007/978-3-319-67474-2_14_references_DOI_D9OVbaNZjyMzJSWnVhOYDK6wJEN"},{"@type":"CROSSREF","@value":"10.1007/s00382-014-2055-2_references_DOI_D9OVbaNZjyMzJSWnVhOYDK6wJEN"},{"@type":"CROSSREF","@value":"10.1029/2018ms001475_references_DOI_D9OVbaNZjyMzJSWnVhOYDK6wJEN"},{"@type":"CROSSREF","@value":"10.5194/acpd-12-29801-2012_references_DOI_D9OVbaNZjyMzJSWnVhOYDK6wJEN"},{"@type":"CROSSREF","@value":"10.5194/gmdd-7-131-2014_references_DOI_D9OVbaNZjyMzJSWnVhOYDK6wJEN"},{"@type":"CROSSREF","@value":"10.1186/s40645-014-0018-1_references_DOI_D9OVbaNZjyMzJSWnVhOYDK6wJEN"},{"@type":"CROSSREF","@value":"10.1186/s40645-020-00351-1_references_DOI_D9OVbaNZjyMzJSWnVhOYDK6wJEN"},{"@type":"CROSSREF","@value":"10.1016/j.envpol.2014.06.006_references_DOI_D9OVbaNZjyMzJSWnVhOYDK6wJEN"}]}