{"created":"2023-07-25T11:04:30.532917+00:00","id":7640,"links":{},"metadata":{"_buckets":{"deposit":"ed08da4d-c044-4660-8c26-5d0fcd72ff33"},"_deposit":{"created_by":4,"id":"7640","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"7640"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00007640","sets":["1259:906:948"]},"author_link":["12073","12075"],"item_1_alternative_title_5":{"attribute_name":"論文名よみ","attribute_value_mlt":[{"subitem_alternative_title":"ショウワ キチ ニオケル ジフブキ ハッセイチュウ ノ シテイ ト フウソク ノ カンケイ ニホン ナンキョク チイキ カンソクタイ ノ ホウコク"}]},"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1971-12","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"42","bibliographicPageStart":"35","bibliographicVolumeNumber":"42","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":"真木, 太一"},{"creatorName":"マキ, タイチ","creatorNameLang":"ja-Kana"}],"nameIdentifiers":[{}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"MAKI, Taichi","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":"At Syowa Station, Antarctica the author investigated the relation between the visibility and the wind velocity from May to August in 1970. On some occasions, blowing snow was mixed in snow fall. The results are summarized as follows ; The snow particles start to drift when the wind velocity at 10m height (U_<10>) becomes larger than 8m/s and the visibility becomes 150m with the wind velocity of about 15m/s ; 10m at about 25m/s ; and 2～3m at about 35m/s. The visibility observed at 1.5m height (V) is inversely proportional to the fifth power of the wind velocity : log (1/V) =5.00×logU_<10>-8.03, where V and U_<10> denote MKS unit. The deduction of friction drag (τ-τ_c) is almost proportional to the fifth power of the velocity (U_<10>). log (τ-τ_c) =5.10×logU_<10>-7.34, where τ is obtained from the friction velocity (U_*), and τ_c from the roughness length (Z_0) of the constant value of 0.01cm. τ, τ_c and U_<10> denote MKS unit. τ, τ_c is related to the energy which causes the blowing of snow particles and is almost inversely proportional to the visibility.","subitem_description_type":"Other"}]},"item_1_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15094/00007640","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_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":"Division of Meteorology, National Institute of Agricultural Sciences"}]},"item_1_text_9":{"attribute_name":"著者所属(日)","attribute_value_mlt":[{"subitem_text_value":"農林省農業技術研究所気象科"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"1971-12-01"}],"displaytype":"detail","filename":"KJ00002476640.pdf","filesize":[{"value":"2.1 MB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"label":"KJ00002476640","url":"https://nipr.repo.nii.ac.jp/record/7640/files/KJ00002476640.pdf"},"version_id":"079b0cdf-bfc8-4150-a342-9136f1d17cab"}]},"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":"昭和基地における地吹雪発生中の視程と風速の関係(日本南極地域観測隊の報告)","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"昭和基地における地吹雪発生中の視程と風速の関係(日本南極地域観測隊の報告)"},{"subitem_title":"Relationship between this Visibility and the Wind Velocity in Drifting Snow at Syowa Station (Reports of the Japanese Antarctic Research Expedition)","subitem_title_language":"en"}]},"item_type_id":"1","owner":"4","path":["948"],"pubdate":{"attribute_name":"公開日","attribute_value":"1971-12-01"},"publish_date":"1971-12-01","publish_status":"0","recid":"7640","relation_version_is_last":true,"title":["昭和基地における地吹雪発生中の視程と風速の関係(日本南極地域観測隊の報告)"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T11:54:00.444947+00:00"}