{"created":"2023-07-25T08:06:23.788865+00:00","id":5145,"links":{},"metadata":{"_buckets":{"deposit":"f703bbd8-156f-4e09-bd3e-0dae5909bc45"},"_deposit":{"created_by":18,"id":"5145","owners":[18],"pid":{"revision_id":0,"type":"depid","value":"5145"},"status":"published"},"_oai":{"id":"oai:ir.kagoshima-u.ac.jp:00005145","sets":["228:259:5382","31:32:93:94"]},"author_link":["109841"],"item_7_biblio_info_5":{"attribute_name":"収録雑誌名","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1983-12-24","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"1","bibliographicPageEnd":"8","bibliographicPageStart":"1","bibliographicVolumeNumber":"4","bibliographic_titles":[{"bibliographic_title":"南海研紀要","bibliographic_titleLang":"ja"},{"bibliographic_title":"Memoirs of the Kagoshima University Research Center for the South Pacific","bibliographic_titleLang":"en"}]}]},"item_7_date_6":{"attribute_name":"作成日","attribute_value_mlt":[{"subitem_date_issued_datetime":"1983-12-24","subitem_date_issued_type":"Issued"}]},"item_7_description_4":{"attribute_name":"要約(Abstract)","attribute_value_mlt":[{"subitem_description":"The annual variation of the north equatorial trough near 15°N and the north\nequatorial countercurrent ridge near 7.5°N in the thermocline topography was investigated by making the 20°C isotherm depth topography in time and space over a six\nyears period. The annual variation in the latitudinal position of the north equatorial\ntrough has an annual cycle, being in the north from November to April and in the\nsouth from May to October. The countercurrent ridge has a semiannual cycle, with the northward shifts from March to April and October to November, and the southward shifts from July to September and December to January, respectively. The annual\nvariation in the depth of both the north equatorial trough and the countercurrent\nridge tends to have an annual cycle, which is deeper from spring to early summer, and\nshallower from fall to winter. The annual variation in dynamic heights and sea levels\nnear 7.5°N in the western tropical Pacific depends partly on the northward and southward shift of the countercurrent ridge in thermocline depths.","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":"03895351","subitem_source_identifier_type":"PISSN"}]},"item_7_source_id_9":{"attribute_name":"NII書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AN00181784","subitem_source_identifier_type":"NCID"}]},"item_7_subject_15":{"attribute_name":"NDC","attribute_value_mlt":[{"subitem_subject":"450","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":"CHAEN, Masaaki","creatorNameLang":"en"},{"creatorName":"茶圓, 正明","creatorNameLang":"ja"}],"nameIdentifiers":[{"nameIdentifier":"109841","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":"2016-10-28"}],"displaytype":"detail","filename":"AN00181784_v4-1_p1-8.pdf","filesize":[{"value":"16.6 MB"}],"format":"application/pdf","mimetype":"application/pdf","url":{"label":"AN00181784_v4-1_p1-8.pdf","objectType":"fulltext","url":"https://ir.kagoshima-u.ac.jp/record/5145/files/AN00181784_v4-1_p1-8.pdf"},"version_id":"bc0469c1-8806-4060-a7f7-38266b46c9dd"}]},"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":"Annual Variation of Thermocline Topography in the Western Tropical Pacific","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Annual Variation of Thermocline Topography in the Western Tropical Pacific","subitem_title_language":"en"}]},"item_type_id":"7","owner":"18","path":["5382","94"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2013-01-22"},"publish_date":"2013-01-22","publish_status":"0","recid":"5145","relation_version_is_last":true,"title":["Annual Variation of Thermocline Topography in the Western Tropical Pacific"],"weko_creator_id":"18","weko_shared_id":-1},"updated":"2024-06-24T08:43:37.314589+00:00"}