{"created":"2023-06-19T11:38:11.724276+00:00","id":5801,"links":{},"metadata":{"_buckets":{"deposit":"73ff54d0-ad02-4967-98d3-b9cf0d23a6af"},"_deposit":{"created_by":13,"id":"5801","owners":[13],"pid":{"revision_id":0,"type":"depid","value":"5801"},"status":"published"},"_oai":{"id":"oai:mie-u.repo.nii.ac.jp:00005801","sets":["420:421:443:457"]},"author_link":["12879","12880"],"item_4_biblio_info_6":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1995-03-25","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"50","bibliographicPageStart":"25","bibliographicVolumeNumber":"14","bibliographic_titles":[{"bibliographic_title":"三重大学生物資源学部紀要 = The bulletin of the Faculty of Bioresources, Mie University"}]}]},"item_4_description_14":{"attribute_name":"フォーマット","attribute_value_mlt":[{"subitem_description":"application/pdf","subitem_description_type":"Other"}]},"item_4_description_4":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"Effect of coastal topography on the western boundary current is studied by use of a barotropic numerical model with special reference to the effect of inclination of the northern boundary from zonal direction. Detailed flow patterns of the numerical experiment are presented in this paper. It is resulted from the numerical experiment that there exists two representative flow pattern: one flow pattern is a meander flow and the other is a straight flow along northern boundary. In case of the meander flow pattern, spin-up and spin-down of the cyclonic eddy accompanied by meander flow are carried out. Meander flow pattern has a tendency to appear in the cases with zonal northern boundary, Chaotic change from meander pattern to straight flow pattern occurs in the case with the inclination of 10° and relatively small eddy viscosity. Straight flow pattern has a tendency to appear in the cases with the large inclination of the northern boundary from zonal direction.","subitem_description_type":"Abstract"},{"subitem_description":"順圧数値モデルを用いて西岸境界流に及ぼす陸岸地形効果に関して，特に東西方向からの北側陸岸境界の傾斜\nの影響を調べた。この論文では得られた結果の詳細な流れのパターンを提示した。数値モデル実験により，蛇行する\n流れのパターンと岸に沿う直進する流れのパターンの二つの代表的なパターンがあることが示された。蛇行する流れ\nのパターンの場合には，蛇行する一般流に伴い低気圧渦が生じ，強化と減衰を繰り返す。蛇行パターンは北側の境界\nが東西の場合に生じる。カオス的な蛇行パターンから直進パターンへの変化が10°の東西方向からの傾斜と相対的\nに小さい渦粘性係数を与えたモデルで発生した。直進する一般流は東西方向からの傾斜が大きい場合に発生する傾向\nが見られた。","subitem_description_type":"Abstract"}]},"item_4_publisher_30":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"Faculty of Bioresources,　Mie University"}]},"item_4_source_id_7":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"0915-0471","subitem_source_identifier_type":"PISSN"}]},"item_4_source_id_9":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AN10073846","subitem_source_identifier_type":"NCID"}]},"item_4_subject_16":{"attribute_name":"日本十進分類法","attribute_value_mlt":[{"subitem_subject":"452","subitem_subject_scheme":"NDC"}]},"item_4_text_18":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_text_language":"ja","subitem_text_value":"西岸境界流に及ぼす陸岸地形効果 : 第1部　陸岸地形の東西からの傾きの影響"}]},"item_4_text_63":{"attribute_name":"ノート","attribute_value_mlt":[{"subitem_text_value":"Agropedia提供データ"}]},"item_4_text_65":{"attribute_name":"資源タイプ（三重大）","attribute_value_mlt":[{"subitem_text_value":"Departmental Bulletin Paper / 紀要論文"}]},"item_4_version_type_15":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_version_resource":"http://purl.org/coar/version/c_970fb48d4fbd8a85","subitem_version_type":"VoR"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Sekine, Yoshihiko","creatorNameLang":"en"},{"creatorName":"関根, 義彦","creatorNameLang":"ja"}],"nameIdentifiers":[{"nameIdentifier":"12879","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Aso, Akiya","creatorNameLang":"en"},{"creatorName":"麻生, 晃也","creatorNameLang":"ja"}],"nameIdentifiers":[{"nameIdentifier":"12880","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":"2017-02-18"}],"displaytype":"detail","filename":"AN100738460001402.pdf","filesize":[{"value":"1.5 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"AN100738460001402.pdf","url":"https://mie-u.repo.nii.ac.jp/record/5801/files/AN100738460001402.pdf"},"version_id":"9bcd044c-9e76-4144-8259-3a35569e1a89"}]},"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":"A Numerical Experiment on the Coastal Effects on the Western Boundary Current : Part I Effect of Inclined Coastline","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"A Numerical Experiment on the Coastal Effects on the Western Boundary Current : Part I Effect of Inclined Coastline","subitem_title_language":"en"}]},"item_type_id":"4","owner":"13","path":["457"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2007-04-25"},"publish_date":"2007-04-25","publish_status":"0","recid":"5801","relation_version_is_last":true,"title":["A Numerical Experiment on the Coastal Effects on the Western Boundary Current : Part I Effect of Inclined Coastline"],"weko_creator_id":"13","weko_shared_id":-1},"updated":"2023-10-12T06:05:20.195909+00:00"}