{"created":"2023-07-25T11:00:58.375580+00:00","id":2885,"links":{},"metadata":{"_buckets":{"deposit":"02d253b7-224c-47a2-9695-5bf5869f63b3"},"_deposit":{"created_by":4,"id":"2885","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"2885"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00002885","sets":["1259:1260:1262:425:427"]},"author_link":["3851","3840","3844","3852","3842","3841","3847","3846","3849","3853","3839","3848","3843","3845","3850"],"item_1_alternative_title_5":{"attribute_name":"論文名よみ","attribute_value_mlt":[{"subitem_alternative_title":"ON THE STRATOSPHERIC OZONE LOSS OVER EUREKA STATION IN THE CANADIAN ARCTIC (II) THE DIFFERENCE BETWEEN 1997/98 AND PREVIOUS YEARS"}]},"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1999-12","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"21","bibliographicPageStart":"11","bibliographicVolumeNumber":"13","bibliographic_titles":[{"bibliographic_title":"Polar meteorology and glaciology"}]}]},"item_1_creator_7":{"attribute_name":"著者名よみ","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"ヒロタ, ミチオ"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"ミヤガワ, コウジ"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"ナガイ, トモヒロ"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"フジモト, トシフミ"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"マキノ, ユキオ"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"ウチノ, オサム"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"アカギ, カズアキ /"}],"nameIdentifiers":[{}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"HIROTA, Michio","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"MIYAGAWA, Koji","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"NAGAI, Tomohiro","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"FUJIMOTO, Toshifumi","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"MAKINO, Yukio","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"UCHINO, Osamu","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"AKAGI, Kazuaki","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"FAST, Hans","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":"Monthly average total ozone and monthly average temperature at 50hPa (T_<50>) over Eureka, both obtained by ECC type ozone sonde observations, were high throughout the winter to early spring of 1997/98 in contrast to those in the former 3 years. The situation is discussed in relation to the relative location of Eureka with respect to the polar vortex boundary and the chemical ozone loss inside the polar vortex. In 1997/98,Eureka was inside the polar vortex in the lower stratosphere (475K potential temperature level) only in the middle of December, early to mid-February and early to mid-March. The period was shorter than in the former 3 years. Moreover, daily T_<50> values when the lower stratosphere over Eureka was inside the polar vortex were not so low compared with those in the former 3 years, and PSCs were not observed over Eureka. The year to year variation of the temperatures in the lower stratosphere (T_<50>) over Eureka inside the polar vortex was generally consistent with the variation of the one within the entire polar vortex. A positive correlation between intravortex potential vorticity (PV) and ozone mixing ratio is expected in the lower stratosphere in the absence of strong chemical ozone loss. In 1997/98,this relation seems to have held during the winter to early spring over Eureka. Also, the total ozone in 1997/98 over Eureka when Eureka was inside the polar vortex in the lower stratosphere was higher than in the former 3 years. These suggest that the chemical ozone loss in 1997/98 inside the polar vortex was small in contrast to the former 3 years.","subitem_description_type":"Other"}]},"item_1_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15094/00002885","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":"AA1129795X","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":"Meteorological College"},{"subitem_text_language":"en","subitem_text_value":"Aerological Observatory"},{"subitem_text_language":"en","subitem_text_value":"Meteorological Research Institute"},{"subitem_text_language":"en","subitem_text_value":"Observations Department, Japan Meteorological Agency"},{"subitem_text_language":"en","subitem_text_value":"Meteorological Research Institute"},{"subitem_text_language":"en","subitem_text_value":"Observations Department, Japan Meteorological Agency"},{"subitem_text_language":"en","subitem_text_value":"Observations Department, Japan Meteorological Agency"},{"subitem_text_language":"en","subitem_text_value":"Atmospheric Environment Service"}]},"item_1_text_3":{"attribute_name":"記事種別(英)","attribute_value_mlt":[{"subitem_text_language":"en","subitem_text_value":"Scientific Paper"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"1999-12-01"}],"displaytype":"detail","filename":"KJ00002409900.pdf","filesize":[{"value":"1.3 MB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"label":"KJ00002409900","url":"https://nipr.repo.nii.ac.jp/record/2885/files/KJ00002409900.pdf"},"version_id":"2f411f2e-28d2-4aa6-a8df-a09c2e73231b"}]},"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":"ON THE STRATOSPHERIC OZONE LOSS OVER EUREKA STATION IN THE CANADIAN ARCTIC (II) THE DIFFERENCE BETWEEN 1997/98 AND PREVIOUS YEARS","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"ON THE STRATOSPHERIC OZONE LOSS OVER EUREKA STATION IN THE CANADIAN ARCTIC (II) THE DIFFERENCE BETWEEN 1997/98 AND PREVIOUS YEARS"}]},"item_type_id":"1","owner":"4","path":["427"],"pubdate":{"attribute_name":"公開日","attribute_value":"1999-12-01"},"publish_date":"1999-12-01","publish_status":"0","recid":"2885","relation_version_is_last":true,"title":["ON THE STRATOSPHERIC OZONE LOSS OVER EUREKA STATION IN THE CANADIAN ARCTIC (II) THE DIFFERENCE BETWEEN 1997/98 AND PREVIOUS YEARS"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T12:41:13.075824+00:00"}