{"created":"2023-07-25T11:04:53.878962+00:00","id":8095,"links":{},"metadata":{"_buckets":{"deposit":"a51f8469-496d-4a8d-81c7-f380bf1c7399"},"_deposit":{"created_by":4,"id":"8095","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"8095"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00008095","sets":["1259:906:973"]},"author_link":["12361","12363"],"item_1_alternative_title_5":{"attribute_name":"論文名よみ","attribute_value_mlt":[{"subitem_alternative_title":"ナンキョク ショウワ キチ デ カンソク サレタ シャメン カコウ フウ ノ エンチョク ブンプ ノ スウチ シミュレーション ダイ1カイ ナンキョク キスイケン シンポジウム"}]},"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1979-10","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"74","bibliographicPageStart":"64","bibliographicVolumeNumber":"67","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":"安達, 隆史"},{"creatorName":"アダチ, タカシ","creatorNameLang":"ja-Kana"}],"nameIdentifiers":[{}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"ADACHI, Takashi","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":"南極昭和基地で観測されたレーウィンソンテのデータのうちで典型的なカタバティック風であると思われる8m/s以上の強風を選んで解析し,風向風速と気温の鉛直分布の特徴を調査したところ,高さが200～300mの層で風速およひ気温が最大になることがわかり,さらにウィント・スパイラルが左まわりになっていることがわかった.そして大気の安定度や温度風と斜面の効果を考慮し,さらに定常で斜面に沿った2次元の一様流を仮定した時に成立する運動方程式系を数値計算によって解いたところ,風速の鉛直分布とウィンド・スパイラルのパターンが実測データと一致する解を得ることがてきた.ただし,この運動方程式系を導入する際には次のような仮定を用いた.すなわち,接地気層で用いられたMonin-Obukhovの相似則をエクマン層全体に拡張する.ただしエクマン層の各高さにおける熱と運動量のフラックスを用いてMonin-Obukhovの長さ(L)は定義されるとし,無次元化風速シャー関数(φ)については中立または安定状態で次式を仮定した.φ=(1+12z/L)^<1/2>","subitem_description_type":"Other"}]},"item_1_description_12":{"attribute_name":"抄録(英)","attribute_value_mlt":[{"subitem_description":"The vertical profiles of the strong katabatic winds at Syowa Station, Antarctica, are studied. A numerical solution of the equations of the Ekman layer above the Antarctic coastal slope is obtained under the following assumptions, (a) The steady state condition (b) The wind component of normal direction to the sloped plane is zero (c) The wind vectors are uniform along the slope at each height (d) Monin-Obukhov's similarity theory is valid in each thin layer of Ekman layer (e) Local value of Monin-Obukhov length is defined by the local heat flux and the local momentum flux (f) New non-dimensional wind shear function (φ) is presented in neutial or stable Ekman laver, φ=(1+12 z/L)^<1/2>","subitem_description_type":"Other"}]},"item_1_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15094/00008095","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":"Research Institute of Japan Weather Association"}]},"item_1_text_9":{"attribute_name":"著者所属(日)","attribute_value_mlt":[{"subitem_text_value":"日本気象協会・研究所"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"1979-10-01"}],"displaytype":"detail","filename":"KJ00002477155.pdf","filesize":[{"value":"1.8 MB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"label":"KJ00002477155","url":"https://nipr.repo.nii.ac.jp/record/8095/files/KJ00002477155.pdf"},"version_id":"4da3d712-5224-4c5e-a71c-88265e88b720"}]},"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":"南極昭和基地で観測された斜面下降風の鉛直分布の数値シミュレーション(第1回南極気水圏シンポジウム)","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"南極昭和基地で観測された斜面下降風の鉛直分布の数値シミュレーション(第1回南極気水圏シンポジウム)"},{"subitem_title":"Numerical Simulation of Katabatic Wind Profile at Syowa Station, Antarctica (Special Issue of the Proceedings of the First Symposium on Antarctic Meteorology and Glaciology)","subitem_title_language":"en"}]},"item_type_id":"1","owner":"4","path":["973"],"pubdate":{"attribute_name":"公開日","attribute_value":"1979-10-01"},"publish_date":"1979-10-01","publish_status":"0","recid":"8095","relation_version_is_last":true,"title":["南極昭和基地で観測された斜面下降風の鉛直分布の数値シミュレーション(第1回南極気水圏シンポジウム)"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T11:48:55.628337+00:00"}