{"created":"2023-07-27T06:52:11.504304+00:00","id":45961,"links":{},"metadata":{"_buckets":{"deposit":"d0d0f367-534e-46d0-989c-883730e848a9"},"_deposit":{"created_by":18,"id":"45961","owners":[18],"pid":{"revision_id":0,"type":"depid","value":"45961"},"status":"published"},"_oai":{"id":"oai:kanazawa-u.repo.nii.ac.jp:00045961","sets":["2812:2813:2815"]},"author_link":["2311","79799"],"item_9_biblio_info_8":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2019-06-19","bibliographicIssueDateType":"Issued"},"bibliographicPageStart":"6p.","bibliographicVolumeNumber":"2014-04-04 - 2019-03-31","bibliographic_titles":[{"bibliographic_title":"平成30(2018)年度 科学研究費補助金 若手研究(A) 研究成果報告書"},{"bibliographic_title":"2018 Fiscal Year Final Research Report","bibliographic_titleLang":"en"}]}]},"item_9_creator_33":{"attribute_name":"著者別表示","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{}],"nameIdentifiers":[{},{}]}]},"item_9_description_21":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"本計画では、東アジア地域における大気エアロゾルの季節変化や増加要因を正確に把握し、その雲凝結核としての働きも含めた物理化学的特性を明らかにするため、能登半島先端の大気観測施設においてエアロゾルの連続観測を行った。\nその結果、季節によって化石燃料と植生の発生源寄与が大きく変化するだけでなく、大陸の森林火災やバイオマスバーニングの影響が、少なからず風下地域のエアロゾルの増加要因となっており、さらには雲凝結核としての活性にも影響していることがわかった。また、従来は主に日中に起こると考えられてきた新粒子生成が、能登では夜間にも確認され、その発生要因として日本海側地域特有の冬季季節風の関与が示唆された。 ","subitem_description_type":"Abstract"},{"subitem_description":"In order to identify the factors controlling the seasonal variation and increasing patterns of atmospheric aerosols in the East Asia region, as well as to clarify the physicochemical characteristics of aerosols including their activity as cloud condensation nuclei, continuous observation was performed at the atmospheric observation facility based at the tip of the Noto Peninsula.\nIt was found that the relative source contribution from fossil fuel and biogenic emissions largely fluctuates depending on the season. Also, forest fire and biomass burning activities in the continent significantly affect the aerosol loading as well as their cloud nucleating ability in the downwind regions. In addition, new particle formation, which was conventionally considered to occur mainly during the daytime, was also spotted at night in Noto, and potential involvement of the unique winter monsoon in the Japan Sea region was suggested as the controlling factor. ","subitem_description_type":"Abstract"}]},"item_9_description_22":{"attribute_name":"内容記述","attribute_value_mlt":[{"subitem_description":"研究課題/領域番号:26701001, 研究期間(年度):2014-04-04 - 2019-03-31","subitem_description_type":"Other"},{"subitem_description":"出典：研究課題「大気中微粒子の増加要因と雲核活性の解明: エアロゾル・クライマトロジー構築にむけて」課題番号26701001\n（KAKEN：科学研究費助成事業データベース（国立情報学研究所）） \n（https://kaken.nii.ac.jp/report/KAKENHI-PROJECT-26701001/26701001seika/)を加工して作成","subitem_description_type":"Other"}]},"item_9_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.24517/00052295","subitem_identifier_reg_type":"JaLC"}]},"item_9_publisher_17":{"attribute_name":"公開者","attribute_value_mlt":[{"subitem_publisher":"金沢大学環日本海域環境研究センター"}]},"item_9_relation_28":{"attribute_name":"関連URI","attribute_value_mlt":[{"subitem_relation_name":[{"subitem_relation_name_text":"https://kaken.nii.ac.jp/search/?qm=90505728"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://kaken.nii.ac.jp/search/?qm=90505728","subitem_relation_type_select":"URI"}},{"subitem_relation_name":[{"subitem_relation_name_text":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-26701001/"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-26701001/","subitem_relation_type_select":"URI"}},{"subitem_relation_name":[{"subitem_relation_name_text":"https://kaken.nii.ac.jp/report/KAKENHI-PROJECT-26701001/26701001seika/"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://kaken.nii.ac.jp/report/KAKENHI-PROJECT-26701001/26701001seika/","subitem_relation_type_select":"URI"}}]},"item_9_version_type_25":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_version_resource":"http://purl.org/coar/version/c_ab4af688f83e57aa","subitem_version_type":"AM"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2020-04-24"}],"displaytype":"detail","filename":"OC-PR-MATSUKI-A-kaken 2019-6p.pdf","filesize":[{"value":"642.7 kB"}],"format":"application/pdf","licensetype":"license_11","mimetype":"application/pdf","url":{"label":"OC-PR-MATSUKI-A-kaken 2019-6p.pdf","url":"https://kanazawa-u.repo.nii.ac.jp/record/45961/files/OC-PR-MATSUKI-A-kaken 2019-6p.pdf"},"version_id":"0576e727-3027-42c9-8330-7f4e75280297"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"jpn"}]},"item_resource_type":{"attribute_name":"資源タイプ","attribute_value_mlt":[{"resourcetype":"research report","resourceuri":"http://purl.org/coar/resource_type/c_18ws"}]},"item_title":"大気中微粒子の増加要因と雲核活性の解明: エアロゾル・クライマトロジー構築にむけて","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"大気中微粒子の増加要因と雲核活性の解明: エアロゾル・クライマトロジー構築にむけて"},{"subitem_title":"Investigation on the source of atmospheric particles are related cloud nucleation activity: Towards the establishment of a new aerosol climatology","subitem_title_language":"en"}]},"item_type_id":"9","owner":"18","path":["2815"],"pubdate":{"attribute_name":"公開日","attribute_value":"2020-04-24"},"publish_date":"2020-04-24","publish_status":"0","recid":"45961","relation_version_is_last":true,"title":["大気中微粒子の増加要因と雲核活性の解明: エアロゾル・クライマトロジー構築にむけて"],"weko_creator_id":"18","weko_shared_id":-1},"updated":"2023-07-27T13:35:50.112009+00:00"}