{"created":"2023-07-25T11:04:08.496484+00:00","id":7171,"links":{},"metadata":{"_buckets":{"deposit":"76c111f0-ddb6-4f70-994f-cb8bc09a75be"},"_deposit":{"created_by":4,"id":"7171","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"7171"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00007171","sets":["1259:906:921","1268:1274"]},"author_link":["11119","10417","11122","10429"],"item_1_alternative_title_5":{"attribute_name":"論文名よみ","attribute_value_mlt":[{"subitem_alternative_title":"ダイ4ジ ナンキョク チイキ カンソクタイ エットウタイ キショウ ブモン ホウコク"}]},"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1962-04","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"1239","bibliographicPageStart":"1229","bibliographicVolumeNumber":"15","bibliographic_titles":[{"bibliographic_title":"南極資料"}]}]},"item_1_creator_6":{"attribute_name":"著者名(日)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"村越, 望"},{"creatorName":"ムラコシ, ノゾミ","creatorNameLang":"ja-Kana"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"矢田, 明"},{"creatorName":"ヤタ, アキラ","creatorNameLang":"ja-Kana"}],"nameIdentifiers":[{}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"MURAKOSHI, Nozomi","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"YATA, Akira","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_11":{"attribute_name":"抄録(日)","attribute_value_mlt":[{"subitem_description":"1961年1月に,第3次越冬隊の気象部門の作業は,第4次越冬隊に引き継がれた.初めてレーウィンゾンデの器械が基地に運ばれ,その設置,調整に約1か月半を要し,3月1日より高層観測が始まり,12月末までに153回観測が行なわれた.過去3回の越冬における地上の月平均気温の最低は,いずれも9月に現われており,春から夏にかけて気温の急上昇を示している.これは成層圏の上層になるに従っても著しい.月平均値による年の振幅は,成層圏の50mbで45℃,地上で25℃に達した.一方対流圏では,各層とも振幅は小であって,10℃位であった.この成層圏の昇温は,上層から次第に下層に及んでいるのがみうけられた.月平均値から計算された昇温率は一般に上層程大きく,100mbで10～11月間に0.5℃/Day,50mbで9～10月間に0.6℃/Dayに達した.気球の破裂高度は冬期に著しく低くなる.この原因として,a)オゾン,酸素の酸化によるゴムの劣化,b)-30℃以下でゴムの張力の喪失,が考えられている.昭和基地においては,気球が-75℃の高度より昇ることは少なかった.これらのことから,ゴムが直接大気に触れないような考慮が払われたら,破裂高度はもっと高くなると思われる.第3次隊の経験では,ゴムを軽油につけて油の膜を作り,飛ばしたが,結果は良かったことが判明した.","subitem_description_type":"Other"}]},"item_1_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15094/00007171","subitem_identifier_reg_type":"JaLC"}]},"item_1_publisher_22":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"国立極地研究所"}]},"item_1_source_id_13":{"attribute_name":"雑誌書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AN00181831","subitem_source_identifier_type":"NCID"}]},"item_1_source_id_20":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"00857289","subitem_source_identifier_type":"ISSN"}]},"item_1_subject_19":{"attribute_name":"米国議会図書館件名標目表","attribute_value_mlt":[{"subitem_subject":"Nihon Nankyoku Chiiki Kansokutai","subitem_subject_scheme":"LCSH"},{"subitem_subject":"Japan. Kishōchō","subitem_subject_scheme":"LCSH"}]},"item_1_subject_21":{"attribute_name":"国際十進分類法","attribute_value_mlt":[{"subitem_subject":"551.5","subitem_subject_scheme":"UDC"}]},"item_1_text_10":{"attribute_name":"著者所属(英)","attribute_value_mlt":[{"subitem_text_language":"en","subitem_text_value":"Japan Meteorological Agency:The Wintering Party, the Japanese Antarctic Research Expeditions, 1956-58 and 1959-61"},{"subitem_text_language":"en","subitem_text_value":"Japan Meteorological Agency:The Japanese Antarctic Research Expedition, 1957-58:The Wintering Party, the Japanese Antarctic Research Expedition, 1959-61"}]},"item_1_text_9":{"attribute_name":"著者所属(日)","attribute_value_mlt":[{"subitem_text_value":"気象庁:第1次,第4次南極地域観測隊越冬隊"},{"subitem_text_value":"気象庁:第2次南極地域観測隊:第4次南極地域観測隊越冬隊"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"1962-04-01"}],"displaytype":"detail","filename":"KJ00002476093.pdf","filesize":[{"value":"1.8 MB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"label":"KJ00002476093","url":"https://nipr.repo.nii.ac.jp/record/7171/files/KJ00002476093.pdf"},"version_id":"5f269c77-4f51-4c78-8d26-4a6636dfdd14"}]},"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":"第4次南極地域観測隊越冬隊気象部門報告","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"第4次南極地域観測隊越冬隊気象部門報告"},{"subitem_title":"Meteorological Observation at Syowa Base during the 4th Wintering","subitem_title_language":"en"}]},"item_type_id":"1","owner":"4","path":["921","1274"],"pubdate":{"attribute_name":"公開日","attribute_value":"1962-04-01"},"publish_date":"1962-04-01","publish_status":"0","recid":"7171","relation_version_is_last":true,"title":["第4次南極地域観測隊越冬隊気象部門報告"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T11:57:34.875532+00:00"}