{"created":"2023-06-19T09:10:49.984870+00:00","id":22383,"links":{},"metadata":{"_buckets":{"deposit":"aa51f880-9b49-4953-96d0-d9f92796c1e2"},"_deposit":{"created_by":1,"id":"22383","owners":[1],"pid":{"revision_id":0,"type":"depid","value":"22383"},"status":"published"},"_oai":{"id":"oai:kumadai.repo.nii.ac.jp:00022383","sets":["405:647","585:629:785"]},"author_link":["154054","154055"],"item_15_alternative_title_22":{"attribute_name":"その他の言語のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"A study on the directional displacement of winter monsoonal surface wind caused by land topography : in the case of northern and southern regions of Kyushu"}]},"item_15_alternative_title_23":{"attribute_name":"タイトル（ヨミ）","attribute_value_mlt":[{"subitem_alternative_title":"セイコウ トウテイ フユガタ キアツ ハイチカ ニ オケル チケイ ニ ヨル フウコウ ヘンイ ニ カンスル ケンキュウ : キュウシュウトウ ホクブ オヨビ ナンブ ノ チジョウフウ ノ バアイ オ チュウシン ト シテ"}]},"item_15_biblio_info_6":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2009-03-10","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"50","bibliographicPageStart":"41","bibliographicVolumeNumber":"100","bibliographic_titles":[{"bibliographic_title":"文学部論叢"}]}]},"item_15_creator_3":{"attribute_name":"別言語の著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Hohgetsu, Takuzo"}],"nameIdentifiers":[{"nameIdentifier":"154055","nameIdentifierScheme":"WEKO"}]}]},"item_15_description_17":{"attribute_name":"フォーマット","attribute_value_mlt":[{"subitem_description":"application/pdf","subitem_description_type":"Other"}]},"item_15_description_46":{"attribute_name":"資源タイプ","attribute_value_mlt":[{"subitem_description":"論文(Article)","subitem_description_type":"Other"}]},"item_15_description_5":{"attribute_name":"内容記述","attribute_value_mlt":[{"subitem_description":"Upper-level and surface sinds generally blow in different each other. This directional displacement is thought to be caused by land topography, and at the same time to cause surface air stream system peculiar to region. Therefore information of the displacement of wind direction at the surface is important to climatological researches on orographic precipitation, for example. The author explained the displacement of winter monsoonal surface wind in northern and southern regions of Kyushu Island, Japan. In this investigation, it developed that main areal distribution of the displacement was divided into five patterns for the northern region, and six patterns for the southern region. These patterns for each region were discriminated one another according to distributions of AMeDAS stations where directional displacements were little or none between surface and upper-level winds.","subitem_description_type":"Other"}]},"item_15_publisher_36":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"熊本大学"}]},"item_15_relation_16":{"attribute_name":"情報源(ISSN)","attribute_value_mlt":[{"subitem_relation_name":[{"subitem_relation_name_text":"03887073"}]}]},"item_15_relation_64":{"attribute_name":"別フォーマットである","attribute_value_mlt":[{"subitem_relation_type":"isFormatOf","subitem_relation_type_id":{"subitem_relation_type_id_text":"http://hdl.handle.net/2298/3285","subitem_relation_type_select":"URI"}}]},"item_15_source_id_9":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AN0022154X","subitem_source_identifier_type":"NCID"}]},"item_15_subject_20":{"attribute_name":"日本十進分類法","attribute_value_mlt":[{"subitem_subject":"454","subitem_subject_scheme":"NDC"}]},"item_15_text_18":{"attribute_name":"形態","attribute_value_mlt":[{"subitem_text_value":"1686116 bytes"}]},"item_15_text_47":{"attribute_name":"資源タイプ・ローカル","attribute_value_mlt":[{"subitem_text_value":"紀要論文"}]},"item_15_text_48":{"attribute_name":"資源タイプ・NII","attribute_value_mlt":[{"subitem_text_value":"Departmental Bulletin Paper"}]},"item_15_text_49":{"attribute_name":"資源タイプ・DCMI","attribute_value_mlt":[{"subitem_text_value":"text"}]},"item_15_text_50":{"attribute_name":"資源タイプ・ローカル表示コード","attribute_value_mlt":[{"subitem_text_value":"02"}]},"item_15_version_type_19":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_version_type":"VoR"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"寶月, 拓三"}],"nameIdentifiers":[{"nameIdentifier":"154054","nameIdentifierScheme":"WEKO"}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2020-03-02"}],"displaytype":"detail","filename":"BR0100_041-050.pdf","filesize":[{"value":"1.7 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"BR0100_041-050.pdf","url":"https://kumadai.repo.nii.ac.jp/record/22383/files/BR0100_041-050.pdf"},"version_id":"e03fd790-bc60-4326-8be4-22890a29960b"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"九州","subitem_subject_scheme":"Other"},{"subitem_subject":"西高東低冬型気圧配置","subitem_subject_scheme":"Other"},{"subitem_subject":"地上風","subitem_subject_scheme":"Other"},{"subitem_subject":"風向偏倚パターン","subitem_subject_scheme":"Other"},{"subitem_subject":"地形条件","subitem_subject_scheme":"Other"}]},"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":"西高東低冬型気圧配置下における地形による風向偏倚に関する研究 : 九州島北部および南部の地上風の場合を中心として","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"西高東低冬型気圧配置下における地形による風向偏倚に関する研究 : 九州島北部および南部の地上風の場合を中心として"}]},"item_type_id":"15","owner":"1","path":["647","785"],"pubdate":{"attribute_name":"公開日","attribute_value":"2009-04-13"},"publish_date":"2009-04-13","publish_status":"0","recid":"22383","relation_version_is_last":true,"title":["西高東低冬型気圧配置下における地形による風向偏倚に関する研究 : 九州島北部および南部の地上風の場合を中心として"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2023-06-19T15:57:42.235161+00:00"}