{"created":"2023-07-25T08:04:08.629519+00:00","id":2260,"links":{},"metadata":{"_buckets":{"deposit":"382cfea2-46f2-4c1c-98a6-1393d387185a"},"_deposit":{"created_by":18,"id":"2260","owners":[18],"pid":{"revision_id":0,"type":"depid","value":"2260"},"status":"published"},"_oai":{"id":"oai:ir.kagoshima-u.ac.jp:00002260","sets":["228:273:5342","35:36"]},"author_link":[],"item_7_biblio_info_5":{"attribute_name":"収録雑誌名","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1980-09","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"194","bibliographicPageStart":"187","bibliographicVolumeNumber":"22","bibliographic_titles":[{"bibliographic_title":"鹿児島大学工学部研究報告","bibliographic_titleLang":"ja"},{"bibliographic_title":"The research reports of the Faculty of Engineering, Kagoshima University","bibliographic_titleLang":"en"}]}]},"item_7_date_6":{"attribute_name":"作成日","attribute_value_mlt":[{"subitem_date_issued_datetime":"1980-09","subitem_date_issued_type":"Issued"}]},"item_7_description_4":{"attribute_name":"要約(Abstract)","attribute_value_mlt":[{"subitem_description":"Current measurements were made on the continental shelf (110m deep) of the East China Sea during several days in Augusts of 1977 and 1978. Tidal currents of M_2 component predominate over other components by a result derived from the measurements by harmonic analysis. The tidal waves of M_2 component are Sverdrup waves progressing to nouth-west under little influence of bottom friction. However, the tidal currents are subject to an influence by a horizontal velocity of semidiurnal internal waves which seems to generate on the continental slope of the East China Sea by coupling with surface tides.","subitem_description_language":"en","subitem_description_type":"Other"}]},"item_7_publisher_23":{"attribute_name":"公開者・出版者","attribute_value_mlt":[{"subitem_publisher":"鹿児島大学","subitem_publisher_language":"ja"},{"subitem_publisher":"Kagoshima University","subitem_publisher_language":"en"}]},"item_7_source_id_7":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"0451212X","subitem_source_identifier_type":"PISSN"}]},"item_7_source_id_9":{"attribute_name":"NII書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AN00040363","subitem_source_identifier_type":"NCID"}]},"item_7_subject_15":{"attribute_name":"NDC","attribute_value_mlt":[{"subitem_subject":"452","subitem_subject_scheme":"NDC"}]},"item_7_version_type_14":{"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":"前田, 明夫","creatorNameLang":"ja"},{"creatorName":"MAEDA, Akio","creatorNameLang":"en"}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2016-10-27"}],"displaytype":"detail","filename":"AN00040363_v22_p187-194.pdf","filesize":[{"value":"834.7 kB"}],"format":"application/pdf","mimetype":"application/pdf","url":{"label":"AN00040363_v22_p187-194.pdf","objectType":"fulltext","url":"https://ir.kagoshima-u.ac.jp/record/2260/files/AN00040363_v22_p187-194.pdf"},"version_id":"d543eae4-579f-42fe-a59c-c760bdc69451"}]},"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":"東シナ海陸棚上成層期におけるM_2分潮流","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"東シナ海陸棚上成層期におけるM_2分潮流","subitem_title_language":"ja"},{"subitem_title":"Tidal currents of M_2 component in a stratified period on the continental self of the East China Sea.","subitem_title_language":"en"}]},"item_type_id":"7","owner":"18","path":["36","5342"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2015-06-10"},"publish_date":"2015-06-10","publish_status":"0","recid":"2260","relation_version_is_last":true,"title":["東シナ海陸棚上成層期におけるM_2分潮流"],"weko_creator_id":"18","weko_shared_id":-1},"updated":"2024-02-20T04:55:58.237549+00:00"}