{"created":"2024-04-08T04:48:07.552773+00:00","id":2001715,"links":{},"metadata":{"_buckets":{"deposit":"c69d84f8-51cb-4ef2-8e14-b3c31562fe67"},"_deposit":{"created_by":10,"id":"2001715","owners":[10],"pid":{"revision_id":0,"type":"depid","value":"2001715"},"status":"published"},"_oai":{"id":"oai:fra.repo.nii.ac.jp:02001715","sets":["12:14:1716950587014"]},"author_link":[],"control_number":"2001715","item_10002_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1990-03","bibliographicIssueDateType":"Issued"},"bibliographicNumberOfPages":"16","bibliographicPageEnd":"24","bibliographicPageStart":"9","bibliographicVolumeNumber":"54","bibliographic_titles":[{"bibliographic_title":"北海道区水産研究所研究報告","bibliographic_titleLang":"ja"},{"bibliographic_title":"Bulletin of the Hokkaido National Fisheries Research Institute","bibliographic_titleLang":"en"}]}]},"item_10002_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"We analyzed the dynamical structure of the Oyashio Region by isobaric surface topographies, based on CTD and direct current measurement data, and examined the relation between cross-/along-stream sea-level difference and the volume transport of the Oyashio Current off southeast coast of Hokkaido. We concluded that the depression of the western Sub-Arctic Circulation and rise of the Sub-Tropical Circulation is substantial but the hump of the Kuroshio Warm Core Ring is subsidiary in the dynamical structure of the Oyashio Region, and that the coastal sea-level difference along the flow can be used as an index of changes in the volume transport along the southeast coast of Hokkaido which is mainly the coastal part of the Oyashio First Branch.","subitem_description_language":"en","subitem_description_type":"Abstract"},{"subitem_description":"CTDデータおよび直接測流データを用いて海面の形状を求めて親潮水域の力学的構造を解析し,道東沖の親潮の流量と水位差との関係を調べた。得られた海面形状は,親潮を含む西部亜寒帯循環の凹部の上に暖水塊に対応する丘状のふくらみが乗る形を示し,暖水塊の隙間から親潮の分枝が貫入しているのではないことを示している。親潮の流れに沿った沿岸の水位差(花咲－十勝)は,親潮第1分枝を主体とする道東沿岸に沿う流れの流量変動の指標となる。しかしこの流れは,対馬暖流などとは異なり,密度躍層の上の低密度水だけに限定されず,大陸斜面および海溝斜面に沿う深い流れであるため,1地点の沿岸水位のみではその流量を指標することはできない。","subitem_description_language":"ja","subitem_description_type":"Abstract"}]},"item_10002_publisher_8":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"北海道区水産研究所","subitem_publisher_language":"ja"},{"subitem_publisher":"Hokkaido National Fisheries Research Institute","subitem_publisher_language":"en"}]},"item_10002_radio_30":{"attribute_name":"作成者","attribute_value_mlt":[{"subitem_radio_item":["吉","田"],"subitem_radio_language":"ja"}]},"item_10002_relation_16":{"attribute_name":"情報源","attribute_value_mlt":[{"subitem_relation_type_id":{"subitem_relation_type_id_text":"hnf_k_54_2","subitem_relation_type_select":"Local"}}]},"item_10002_relation_17":{"attribute_name":"関連サイト","attribute_value_mlt":[{"subitem_relation_name":[{"subitem_relation_name_language":"ja","subitem_relation_name_text":"日本農学文献記事索引(agriknowledge)"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://agriknowledge.affrc.go.jp/RN/2010460898","subitem_relation_type_select":"URI"}}]},"item_10002_source_id_11":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AN1015410X","subitem_source_identifier_type":"NCID"}]},"item_10002_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"0513-2541","subitem_source_identifier_type":"PISSN"}]},"item_access_right":{"attribute_name":"アクセス権","attribute_value_mlt":[{"subitem_access_right":"metadata only access","subitem_access_right_uri":"http://purl.org/coar/access_right/c_14cb"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"柏井, 誠","creatorNameLang":"ja"},{"creatorName":"カシワイ, マコト","creatorNameLang":"ja-Kana"},{"creatorName":"Kashiwai, Makoto","creatorNameLang":"en"}],"familyNames":[{"familyName":"柏井","familyNameLang":"ja"},{"familyName":"カシワイ","familyNameLang":"ja-Kana"},{"familyName":"Kashiwai","familyNameLang":"en"}],"givenNames":[{"givenName":"誠","givenNameLang":"ja"},{"givenName":"マコト","givenNameLang":"ja-Kana"},{"givenName":"Makoto","givenNameLang":"en"}]},{"creatorNames":[{"creatorName":"河野, 時廣","creatorNameLang":"ja"},{"creatorName":"コウノ, トキヒロ","creatorNameLang":"ja-Kana"},{"creatorName":"Kono, Tokihiro","creatorNameLang":"en"}],"familyNames":[{"familyName":"河野","familyNameLang":"ja"},{"familyName":"コウノ","familyNameLang":"ja-Kana"},{"familyName":"Kono","familyNameLang":"en"}],"givenNames":[{"givenName":"時廣","givenNameLang":"ja"},{"givenName":"トキヒロ","givenNameLang":"ja-Kana"},{"givenName":"Tokohiro","givenNameLang":"en"}]}]},"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":"海面形状および水位差と親潮の流量変動との関係","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"海面形状および水位差と親潮の流量変動との関係","subitem_title_language":"ja"},{"subitem_title":"Surface topography, sea-level difference and volume transport of the Oyashio Current","subitem_title_language":"en"}]},"item_type_id":"10002","owner":"10","path":["1716950587014"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2024-04-08"},"publish_date":"2024-04-08","publish_status":"0","recid":"2001715","relation_version_is_last":true,"title":["海面形状および水位差と親潮の流量変動との関係"],"weko_creator_id":"10","weko_shared_id":-1},"updated":"2025-01-20T05:07:05.100863+00:00"}