{"created":"2023-07-25T11:01:34.965826+00:00","id":3638,"links":{},"metadata":{"_buckets":{"deposit":"6b52e4d3-573d-4430-ab55-de84e40c8461"},"_deposit":{"created_by":4,"id":"3638","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"3638"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00003638","sets":["1259:1260:1262:524:528"]},"author_link":["5237","5236","5235","5234"],"item_1_alternative_title_5":{"attribute_name":"論文名よみ","attribute_value_mlt":[{"subitem_alternative_title":"NITRIC ACID TRANSPORT FROM THE STRATOSPHERE TO THE TROPOSPHERE AND ICE SHEET IN ANTARCTICA THROUGH POLAR STRATOSPHERE"}]},"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1991-05","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"21","bibliographicPageStart":"12","bibliographicVolumeNumber":"4","bibliographic_titles":[{"bibliographic_title":"Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology"}]}]},"item_1_creator_7":{"attribute_name":"著者名よみ","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"イワサカ, ヤスノブ"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"ハヤシ, マサヒコ"}],"nameIdentifiers":[{}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"IWASAKA, Yasunobu","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"HAYASHI, Masahiko","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":"Growth and sedimentation of polar stratospheric clouds (PSCs) particles are examined using a numerical model named the 'Test Particle Sedimentation Model'.PSCs particles transport stratospheric nitric acid (HNO_3) to the troposphere (maybe near the ice sheet) for several days by their sedimentation. The amounts of HNO_3 and H_2O removed by a particle depends on the trajectory of the particle (length of path and residence time). Usually the removed amount is larger in the higher part of the PSCs layer comparing with the lower part of the layer. The features of HNO_3 transport are consistent with the results of chemical analyses of the Antarctic ice sheet and of aerosols sampled at the surface of the ice sheet.","subitem_description_type":"Other"}]},"item_1_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15094/00003638","subitem_identifier_reg_type":"JaLC"}]},"item_1_publisher_22":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"National Institute of Polar Research"}]},"item_1_source_id_13":{"attribute_name":"雑誌書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AA10756213","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":"Solar Terrestrial Environment Laboratory, Nagoya University"},{"subitem_text_language":"en","subitem_text_value":"Water Research Institute, Nagoya University:Solar Terrestrial Environment Laboratory, 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":"1991-05-01"}],"displaytype":"detail","filename":"KJ00000767841.pdf","filesize":[{"value":"1.5 MB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"label":"KJ00000767841","url":"https://nipr.repo.nii.ac.jp/record/3638/files/KJ00000767841.pdf"},"version_id":"d9f222be-a53d-4b0a-a891-4a25062c74da"}]},"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":"NITRIC ACID TRANSPORT FROM THE STRATOSPHERE TO THE TROPOSPHERE AND ICE SHEET IN ANTARCTICA THROUGH POLAR STRATOSPHERE","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"NITRIC ACID TRANSPORT FROM THE STRATOSPHERE TO THE TROPOSPHERE AND ICE SHEET IN ANTARCTICA THROUGH POLAR STRATOSPHERE"}]},"item_type_id":"1","owner":"4","path":["528"],"pubdate":{"attribute_name":"公開日","attribute_value":"1991-05-01"},"publish_date":"1991-05-01","publish_status":"0","recid":"3638","relation_version_is_last":true,"title":["NITRIC ACID TRANSPORT FROM THE STRATOSPHERE TO THE TROPOSPHERE AND ICE SHEET IN ANTARCTICA THROUGH POLAR STRATOSPHERE"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T12:31:11.828859+00:00"}