{"created":"2023-07-25T11:00:17.259016+00:00","id":2071,"links":{},"metadata":{"_buckets":{"deposit":"e6260e7a-5e95-44ce-a8f7-e9be4e3df0fa"},"_deposit":{"created_by":4,"id":"2071","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"2071"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00002071","sets":["1:356:399"]},"author_link":["1672"],"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1986-12","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"18","bibliographicPageStart":"13","bibliographicVolumeNumber":"45","bibliographic_titles":[{"bibliographic_title":"Memoirs of National Institute of Polar Research. Special issue"}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Iwasaka, Yasunobu","creatorNameLang":"en"}],"nameIdentifiers":[{}]}]},"item_1_description_1":{"attribute_name":"ページ属性","attribute_value_mlt":[{"subitem_description":"P(論文)","subitem_description_type":"Other"}]},"item_1_description_12":{"attribute_name":"抄録(英)","attribute_value_mlt":[{"subitem_description":"Lidar measurements at Syowa Station (69°00′S, 39°35′E) revealed that the centroid of aerosol layer descended at the rate of 0.8mm/s during winter. If this motion is a substantial movement of aerosol particles, the mass of water transported into the troposphere is about 5×(10)^7t/winter, and the Antarctic winter stratosphere is an important sink of stratospheric water vapor. If it is a downword air motion carrying small ice crystals, the value is reduced to 5×(10)^4t/winter.","subitem_description_type":"Other"}]},"item_1_source_id_13":{"attribute_name":"雑誌書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AA00733561","subitem_source_identifier_type":"NCID"}]},"item_1_text_10":{"attribute_name":"著者所属(英)","attribute_value_mlt":[{"subitem_text_language":"en","subitem_text_value":"Water Research Institute, Nagoya University"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"1986-12-01"}],"displaytype":"detail","filename":"KJ00000012624.pdf","filesize":[{"value":"1.1 MB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"url":"https://nipr.repo.nii.ac.jp/record/2071/files/KJ00000012624.pdf"},"version_id":"0ca685f7-2152-480b-bbd6-6890569b0239"}]},"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":"departmental bulletin paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"Descending motion of Antarctic stratospheric aerosol layer in winter: Possible effect on stratospheric water vapor budget","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Descending motion of Antarctic stratospheric aerosol layer in winter: Possible effect on stratospheric water vapor budget","subitem_title_language":"en"}]},"item_type_id":"1","owner":"4","path":["399"],"pubdate":{"attribute_name":"公開日","attribute_value":"1986-12-01"},"publish_date":"1986-12-01","publish_status":"0","recid":"2071","relation_version_is_last":true,"title":["Descending motion of Antarctic stratospheric aerosol layer in winter: Possible effect on stratospheric water vapor budget"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T13:44:47.295395+00:00"}