{"created":"2023-06-19T11:38:17.719743+00:00","id":5938,"links":{},"metadata":{"_buckets":{"deposit":"08cd84c8-d868-4723-b747-0e13284adea7"},"_deposit":{"created_by":13,"id":"5938","owners":[13],"pid":{"revision_id":0,"type":"depid","value":"5938"},"status":"published"},"_oai":{"id":"oai:mie-u.repo.nii.ac.jp:00005938","sets":["420:421:443:471"]},"author_link":["13385","13386"],"item_4_biblio_info_6":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2003-03-15","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"56","bibliographicPageStart":"47","bibliographicVolumeNumber":"30","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":"西岸境界流の水平流速分布を知るために,1992年7月から2001年8月までに日本南岸の黒潮を横切るADCP観測を6回行った。この論文ではこれらの観測で得られたADCP流速の分布を提示する。日本南岸の岸近くでは黒潮流速が顕著に減少することが共通して観測され,数値モデルについては粘性の境界条件が適切であり,非粘性境界条件や超非粘性境界条件さらに極粘性境界条件のような岸近くで最大速度となる条件は不適切であることが示された。2001年8月にはわずか2日の間に極めて著しい流れの変化を観測し,黒潮に及ぼす顕著な伊豆海嶺の地形効果が示唆された。順圧流に対して伊豆小笠原海溝の地形効果は小さく,南西諸島東の陸棚斜面から北緯31度の伊豆海嶺の南端を結ぶ海流の存在が示唆された。これらの観測結果を基礎に,1992年以降の観測期間では離岸型非大蛇行流路が卓越することの背景を議論した。","subitem_description_type":"Abstract"},{"subitem_description":"In order to see horizontal distribution of the velocity across the western boundary current, we have made six ADCP observations across the Kuroshio south of Japan over the period from July 1992 to August 2001. Observed ADCP velocity distribution across the Kuroshio is given in the present paper. It is shown that almost all the observed ADCP velocities decreased significantly in the nearshore coastal regions of Japan, which suggests that the viscous coastal boundary condition for numerical models of the Kuroshio is more suitable than some slippery conditions with the maximum velocity at the coastal boundary, such as the slip boundary, superslip and hyperslip boundary conditions. It is also shown that in August 2001, a prominent time change in the velocity distribution south of the mean flow of the Kuroshio was observed during only two days, in which the strong topographic effect of the Izu Ridge on the variation in the Kuroshio main axis is detected. The topographic effect of the Izu-Ogasawara Trench is shown to be small, and a barotropic current from the continental slope of the Nansei Islands to south of the Izu Ridge at latitude of 31°N is suggested. On the basis of the observed ADCP data, the dominant appearance of the offshore non-large meander path of the Kuroshio since 1992 is discussed.","subitem_description_type":"Abstract"}]},"item_4_description_5":{"attribute_name":"内容記述","attribute_value_mlt":[{"subitem_description":"原著論文 / Original Article","subitem_description_type":"Other"}]},"item_4_publisher_30":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"三重大学生物資源学部"}]},"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":"en","subitem_text_value":"Observation on the ADCP velocity of the Kuroshio south of Japan"}]},"item_4_text_63":{"attribute_name":"ノート","attribute_value_mlt":[{"subitem_text_value":"NII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":"関根, 義彦","creatorNameLang":"ja"},{"creatorName":"セキネ, ヨシヒコ","creatorNameLang":"ja-Kana"},{"creatorName":"SEKINE, Yoshihiko","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"山田, 二久次","creatorNameLang":"ja"},{"creatorName":"ヤマダ, フクジ","creatorNameLang":"ja-Kana"},{"creatorName":"YAMADA, Fukuji","creatorNameLang":"en"}],"nameIdentifiers":[{}]}]},"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":"KJ00000693327.pdf","filesize":[{"value":"794.6 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"KJ00000693327.pdf","url":"https://mie-u.repo.nii.ac.jp/record/5938/files/KJ00000693327.pdf"},"version_id":"bf8d5cd0-c38f-4b96-ac08-dc2a99f4e7b4"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"Kuroshio","subitem_subject_scheme":"Other"},{"subitem_subject":"current velocity","subitem_subject_scheme":"Other"},{"subitem_subject":"horizontal velocity shear","subitem_subject_scheme":"Other"}]},"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":"日本南岸の黒潮のADCP流速観測","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"日本南岸の黒潮のADCP流速観測","subitem_title_language":"ja"}]},"item_type_id":"4","owner":"13","path":["471"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2007-02-09"},"publish_date":"2007-02-09","publish_status":"0","recid":"5938","relation_version_is_last":true,"title":["日本南岸の黒潮のADCP流速観測"],"weko_creator_id":"13","weko_shared_id":-1},"updated":"2023-10-13T01:29:59.052323+00:00"}