{"created":"2023-05-15T13:44:40.861749+00:00","id":1248,"links":{},"metadata":{"_buckets":{"deposit":"c35e426f-a26e-4e04-9281-27a6a6dc2d73"},"_deposit":{"created_by":1,"id":"1248","owners":[1],"pid":{"revision_id":0,"type":"depid","value":"1248"},"status":"published"},"_oai":{"id":"oai:chuo-u.repo.nii.ac.jp:00001248","sets":["108:116"]},"author_link":["23379","23732","23734","23727","23730","23736","23725","23733","23728","23735","23726","23731","23729"],"item_10002_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2004-03-31","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"42","bibliographicPageStart":"31","bibliographicVolumeNumber":"9","bibliographic_titles":[{"bibliographic_title":"中央大学理工学研究所論文集"}]}]},"item_10002_description_19":{"attribute_name":"フォーマット","attribute_value_mlt":[{"subitem_description":"application/pdf","subitem_description_type":"Other"}]},"item_10002_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"本研究は，実スケールの雲物理実験から雲及び雨の生成過程を詳細に捉え，エアロゾルが降雨現象に与える影響を解明するとともに，その結果を反映した新たな降雨モデルの構築を行うことを目的としている．ここでは，雨粒が溶液であることにより飽和水蒸気圧が変化する効果を降雨モデルに取り入れ，エアロゾルの化学組成が雲及び雨の生成に与える影響と実験よりエアロゾルの数濃度が雲粒への凝結成長過程を明らかにする．","subitem_description_type":"Abstract"}]},"item_10002_description_6":{"attribute_name":"内容記述","attribute_value_mlt":[{"subitem_description":"【査読有】","subitem_description_type":"Other"}]},"item_10002_full_name_32":{"attribute_name":"著者別名(英)","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"23379","nameIdentifierScheme":"WEKO"}],"names":[{"name":"YAMADA, 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