{"created":"2023-07-25T11:05:39.117829+00:00","id":8966,"links":{},"metadata":{"_buckets":{"deposit":"6036c84d-4006-4a4e-a1a7-d3d0da8debec"},"_deposit":{"created_by":4,"id":"8966","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"8966"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00008966","sets":["1259:906:1236:1116"]},"author_link":["15762","15760"],"item_1_alternative_title_5":{"attribute_name":"論文名よみ","attribute_value_mlt":[{"subitem_alternative_title":"キャッカン カイセキ データ ニヨル ナンキョクイキ ニオケル タイキチュウ ノ ミズジュンカン ノ キセツ ヘンカ"}]},"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1997-03","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"1","bibliographicPageEnd":"160","bibliographicPageStart":"149","bibliographicVolumeNumber":"41","bibliographic_titles":[{"bibliographic_title":"南極資料"},{"bibliographic_title":"Antarctic Record","bibliographic_titleLang":"en"}]}]},"item_1_creator_6":{"attribute_name":"著者名(日)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"山崎, 孝治"},{"creatorName":"ヤマザキ, コウジ","creatorNameLang":"ja-Kana"}],"nameIdentifiers":[{}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Yamazaki, Koji","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":"地球上で最も水蒸気の少ない南極域の大気中の水循環を調べる目的で, 6年間(1986-1991年)の1日2回の米国NMCの客観解析データから可降水量, 全水蒸気フラックス及びその収束量を計算した。可降水量は夏に多いが, 帯状平均極向き水蒸気フラックス及びその収束(「降水量-蒸発量」に対応する)は冬に多く, 半年振動も見られる。これは水蒸気フラックス及びその収束の季節変化は, 南極域では主に低気圧活動に支配されていることの反映である。南緯70度より極側では北極域では見られない西向きの水蒸気フラックスが大陸沿岸を中心に見られ, 特に夏に顕著である。また, 南極域の水循環は, 全球平均と比べて活発で, 特に冬には顕著であることもわかった。","subitem_description_type":"Other"}]},"item_1_description_12":{"attribute_name":"抄録(英)","attribute_value_mlt":[{"subitem_description":"Precipitable water, total moisture flux and its convergence are calculated based on the 6-year (1986-1991) twice-daily U.S. NMC data to investigate the atmospheric water circulation in the Antarctic region. The precipitable water becomes large in summer, but the zonal mean poleward moisture flux and its convergence, which corresponds to \"precipitation minus evaporation\", become large in winter and they also exhibit semi-annual variation. This is because the seasonal variation of moisture flux and its convergence is mainly controlled by the cyclonic activity in the Antarctic region. The westward moisture flux, which does not exist in the Arctic region, is seen poleward of 70° along the Antarctic continent and it is significant in summer. It is found that the atmospheric water circulation in the Antarctic region is very active compared with the global mean, especially in winter.","subitem_description_type":"Other"}]},"item_1_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15094/00008966","subitem_identifier_reg_type":"JaLC"}]},"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_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":"Graduate School of Environmental Earth Science,Hokkaido University"}]},"item_1_text_9":{"attribute_name":"著者所属(日)","attribute_value_mlt":[{"subitem_text_value":"北海道大学大学院地球環境科学研究科"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"1997-03-01"}],"displaytype":"detail","filename":"KJ00000140315.pdf","filesize":[{"value":"412.1 kB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"label":"KJ00000140315","url":"https://nipr.repo.nii.ac.jp/record/8966/files/KJ00000140315.pdf"},"version_id":"ff24f6b1-3186-49de-8c63-a854caf59f66"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"jpn"}]},"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":"客観解析データによる南極域における大気中の水循環の季節変化","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"客観解析データによる南極域における大気中の水循環の季節変化"},{"subitem_title":"Seasonal variation of atmospheric water circulation in the Antarctic region derived from objective analysis data","subitem_title_language":"en"}]},"item_type_id":"1","owner":"4","path":["1116"],"pubdate":{"attribute_name":"公開日","attribute_value":"1997-03-01"},"publish_date":"1997-03-01","publish_status":"0","recid":"8966","relation_version_is_last":true,"title":["客観解析データによる南極域における大気中の水循環の季節変化"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T13:13:51.314319+00:00"}