{"created":"2023-07-25T11:09:26.105827+00:00","id":13462,"links":{},"metadata":{"_buckets":{"deposit":"db53f22e-6da8-4836-9710-93f4d6c6cfd3"},"_deposit":{"created_by":4,"id":"13462","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"13462"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00013462","sets":["1497:1502:1697"]},"author_link":["41810","41807","41808","41809"],"item_2_date_7":{"attribute_name":"発表年月日","attribute_value_mlt":[{"subitem_date_issued_datetime":"2011-11-14","subitem_date_issued_type":"Issued"}]},"item_2_description_6":{"attribute_name":"会議概要(会議名, 開催地, 会期, 主催者等)","attribute_value_mlt":[{"subitem_description":"第2回極域科学シンポジウム/第35回極域宙空圏シンポジウム \n11月14日(月) 国立極地研究所 2階大会議室","subitem_description_type":"Other"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"高麗, 正史"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"佐藤, 薫"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"M., Kohma","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"K., Sato","creatorNameLang":"en"}],"nameIdentifiers":[{}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2016-08-30"}],"displaytype":"detail","filename":"C_AU03_KohmaMasashi.pdf","filesize":[{"value":"436.5 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"C_AU03_KohmaMasashi.pdf","url":"https://nipr.repo.nii.ac.jp/record/13462/files/C_AU03_KohmaMasashi.pdf"},"version_id":"aada16c5-8767-4e59-b5fa-5c1a5d636c07"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"eng"}]},"item_resource_type":{"attribute_name":"資源タイプ","attribute_value_mlt":[{"resourcetype":"conference object","resourceuri":"http://purl.org/coar/resource_type/c_c94f"}]},"item_title":"極成層圏雲と上部対流圏の雲との関係 -ブロッキングの役割-","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"極成層圏雲と上部対流圏の雲との関係 -ブロッキングの役割-"},{"subitem_title":"The relationship between polar stratospheric clouds and upper tropospheric clouds -the role of blocking highs-","subitem_title_language":"en"}]},"item_type_id":"2","owner":"4","path":["1697"],"pubdate":{"attribute_name":"公開日","attribute_value":"2016-08-30"},"publish_date":"2016-08-30","publish_status":"0","recid":"13462","relation_version_is_last":true,"title":["極成層圏雲と上部対流圏の雲との関係 -ブロッキングの役割-"],"weko_creator_id":"4","weko_shared_id":-1},"updated":"2023-07-25T15:49:07.246596+00:00"}