{"created":"2023-07-25T08:10:39.852767+00:00","id":10639,"links":{},"metadata":{"_buckets":{"deposit":"a7840972-49e7-4d3c-a1c3-6d6ae9e21368"},"_deposit":{"created_by":18,"id":"10639","owners":[18],"pid":{"revision_id":0,"type":"depid","value":"10639"},"status":"published"},"_oai":{"id":"oai:ir.kagoshima-u.ac.jp:00010639","sets":["228:262:4720","39:40"]},"author_link":["16733","12086","104491","12954"],"item_7_biblio_info_5":{"attribute_name":"収録雑誌名","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1990-12-25","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"66","bibliographicPageStart":"49","bibliographicVolumeNumber":"39","bibliographic_titles":[{"bibliographic_title":"鹿児島大学水産学部紀要","bibliographic_titleLang":"ja"},{"bibliographic_title":"Memoirs of Faculty of Fisheries Kagoshima University","bibliographic_titleLang":"en"}]}]},"item_7_date_6":{"attribute_name":"作成日","attribute_value_mlt":[{"subitem_date_issued_datetime":"1990-12-25","subitem_date_issued_type":"Issued"}]},"item_7_description_4":{"attribute_name":"要約(Abstract)","attribute_value_mlt":[{"subitem_description":"Using CTD data obtained on the T/S Kagoshima-maru during 20 hours on December 2-3, 1989 in a triangular area centered at 29-09N, 134-51E (each distance between three tips are 35 miles), the small scale spatial distribution of ocean surface mixed layer depth (MLD) and the vertical heat flux at the bottom of surface mixed layer were examined. Assuming the spatial homogeneousness of internal tide, the contribution of internal tide to MLD defined by sea surface temperature (SST) minus 1.0°C depth, is estimated to ±20m, about 20% of mean MLD. Spatial distribution of MLD corrected by reducing the internal tidal components by least square method has good similarity with temperature distribution at 200m depth, suggesting that MLD distribution is well correlated with two cyclonic small eddies at 200m depth of which radii are 15-40 miles. Vertical velocity component of the current flowing along isopycnal surface at 100m depth is calculated to be 2.2×10^{-3} cm s^{-1} by beta-spiral method using CTD data which does not contain the contribution of internal tide but eddy. Then, vertical heat flux (positive upward) at the bottom of surface mixed layer (100m depth) was estimated to be -78W m^{-2} using mean temperatures at 75 and 100m depth.","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":"0453087X","subitem_source_identifier_type":"PISSN"}]},"item_7_source_id_9":{"attribute_name":"NII書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AN00040498","subitem_source_identifier_type":"NCID"}]},"item_7_subject_15":{"attribute_name":"NDC","attribute_value_mlt":[{"subitem_subject":"663","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":"市川, 洋","creatorNameLang":"ja"},{"creatorName":"ICHIKAWA, Hiroshi","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"16733","nameIdentifierScheme":"WEKO"},{"nameIdentifier":"1000060128410","nameIdentifierScheme":"NRID","nameIdentifierURI":" "}]},{"creatorNames":[{"creatorName":"茶圓, 正明","creatorNameLang":"ja"},{"creatorName":"CHAEN, Masaaki","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"12086","nameIdentifierScheme":"WEKO"},{"nameIdentifier":"1000030041700","nameIdentifierScheme":"NRID","nameIdentifierURI":" "}]},{"creatorNames":[{"creatorName":"内山, 正樹","creatorNameLang":"ja"},{"creatorName":"UCHIYAMA, Masaki","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"104491","nameIdentifierScheme":"WEKO"}]},{"creatorAlternatives":[{"creatorAlternative":"日髙, 正康","creatorAlternativeLang":"ja"}],"creatorNames":[{"creatorName":"日高, 正康","creatorNameLang":"ja"},{"creatorName":"HIDAKA, Masayasu","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"12954","nameIdentifierScheme":"WEKO"},{"nameIdentifier":"1000020208771","nameIdentifierScheme":"NRID","nameIdentifierURI":" "}]}]},"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":"AN00040498_v39_p49-66.pdf","filesize":[{"value":"1.5 MB"}],"format":"application/pdf","mimetype":"application/pdf","url":{"label":"AN00040498_v39_p49-66.pdf","objectType":"fulltext","url":"https://ir.kagoshima-u.ac.jp/record/10639/files/AN00040498_v39_p49-66.pdf"},"version_id":"15f963a6-20be-4d14-8b08-fd30ebcf58ef"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"Air-sea interaction","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Ocean mixed layer","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Heat flux","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Heat advection","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Beta-spiral","subitem_subject_language":"en","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":"海洋表層混合層厚微細分布と混合層底面での鉛直熱輪送","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"海洋表層混合層厚微細分布と混合層底面での鉛直熱輪送","subitem_title_language":"ja"},{"subitem_title":"Small scale distribution of surface mixed layer depth and vertical heat advection at the bottom of mixed layer","subitem_title_language":"en"}]},"item_type_id":"7","owner":"18","path":["40","4720"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2015-06-04"},"publish_date":"2015-06-04","publish_status":"0","recid":"10639","relation_version_is_last":true,"title":["海洋表層混合層厚微細分布と混合層底面での鉛直熱輪送"],"weko_creator_id":"18","weko_shared_id":-1},"updated":"2024-07-30T01:13:01.805939+00:00"}