{"created":"2024-04-25T05:05:53.013833+00:00","id":2003269,"links":{},"metadata":{"_buckets":{"deposit":"f7e24076-f2e0-445f-9d7d-93b1a192aef9"},"_deposit":{"created_by":10,"id":"2003269","owners":[10],"pid":{"revision_id":0,"type":"depid","value":"2003269"},"status":"published"},"_oai":{"id":"oai:fra.repo.nii.ac.jp:02003269","sets":["12:14:1716951205920"]},"author_link":["3337"],"control_number":"2003269","item_10002_biblio_info_7":{"attribute_name":"bibliographic_information","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1985-02","bibliographicIssueDateType":"Issued"},"bibliographicNumberOfPages":"11","bibliographicPageEnd":"49","bibliographicPageStart":"39","bibliographicVolumeNumber":"18","bibliographic_titles":[{"bibliographic_title":"南西海区水産研究所研究報告","bibliographic_titleLang":"ja"},{"bibliographic_title":"Bulletin of the Nansei Regional Fisheries Research Laboratory","bibliographic_titleLang":"en"}]}]},"item_10002_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"The Kuroshio flow South of Japan which essentially governs the oceanographic condition in Nansei Coastal Region including Kii and Bungo Straits can be subdivided into two patterns: the Kuroshio with meander (A pattern-A period) and the Kuroshio with no meander (B, C, D, N pattern-N period). The difference between the two mean temperatures in and outside of Kii Strait, which were averaged individually in A (July 1975 - Dec. 1979) and N (Jan. 1970 – June 1975) period, was discussed. The results were as follows. 1. Generally the mean temperature during A period are slightly lower than that during N period. But the appearance of this slightly lower temperature is very complicated and unsystematic in time and space.  2. This complexity in this region may be caused by the short period fluctuations of the Kuroshio which are more dominant during A period than N period. 3. In Kii Strait and adjacent seas, it is recommended to calculate mean temperatures individually in the period of A and N period and to use properly according to the demand.","subitem_description_language":"en","subitem_description_type":"Abstract"},{"subitem_description":"紀伊·豊後両水道を含む南西海区沿岸域の海況を基本的に支配する黒潮は,大蛇行流路(A型流路 - A型期)と非蛇行流路(B,C,D,N型流路 - N型期)の二つに分けることができる。ここでは,紀伊水道及びその外域において,A型期(1975年7月~1979年12月)とN型期(1970年1月~1975年6月)別に求めた平均水温差について検討した。得られた結果は,次の通りである。1. 全般的にみてA型期の平均水温は,N型期よりやや低い傾向にある。しかし,低温傾向の出現は非常に複雑で系統的でない。2. 当海域でみられる平均水温差の複雑さは,N型期よりA型期に,より卓越する黒潮の短期変動によるものと思われる。3. 紀伊水道及びその外域では,海況別(黒潮の蛇行,非蛇行)に平均値を求め,用途に応じて使い分ける必要がある。","subitem_description_language":"ja","subitem_description_type":"Abstract"}]},"item_10002_publisher_8":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"南西海区水産研究所","subitem_publisher_language":"ja"},{"subitem_publisher":"Nansei Regional Fisheries Research Laboratory","subitem_publisher_language":"en"}]},"item_10002_radio_30":{"attribute_name":"item_10002_radio_30","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":"nnf_k_18_39","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/2010824231","subitem_relation_type_select":"URI"}}]},"item_10002_source_id_11":{"attribute_name":"item_10002_source_id_11","attribute_value_mlt":[{"subitem_source_identifier":"AN00181988","subitem_source_identifier_type":"NCID"}]},"item_10002_source_id_9":{"attribute_name":"item_10002_source_id_9","attribute_value_mlt":[{"subitem_source_identifier":"0388-841X","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":"Sakamoto, Hisao","creatorNameLang":"en","creatorNameType":"Personal"},{"creatorName":"坂本, 久雄","creatorNameLang":"ja","creatorNameType":"Personal"},{"creatorName":"サカモト, ヒサオ","creatorNameLang":"ja-Kana","creatorNameType":"Personal"}],"familyNames":[{"familyName":"Sakamoto","familyNameLang":"en"},{"familyName":"坂本","familyNameLang":"ja"},{"familyName":"サカモト","familyNameLang":"ja-Kana"}],"givenNames":[{"givenName":"Hisao","givenNameLang":"en"},{"givenName":"久雄","givenNameLang":"ja"},{"givenName":"ヒサオ","givenNameLang":"ja-Kana"}],"nameIdentifiers":[{"nameIdentifier":"3337","nameIdentifierScheme":"WEKO"}]}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"jpn"}]},"item_resource_type":{"attribute_name":"item_resource_type","attribute_value_mlt":[{"resourcetype":"departmental bulletin paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"紀伊水道及びその外域における黒潮蛇行期と非蛇行期の平均水温について","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"紀伊水道及びその外域における黒潮蛇行期と非蛇行期の平均水温について","subitem_title_language":"ja"},{"subitem_title":"Mean Temperature in and outside of Kii Strait during the Kuroshio with and without Meander","subitem_title_language":"en"}]},"item_type_id":"10002","owner":"10","path":["1716951205920"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2024-04-25"},"publish_date":"2024-04-25","publish_status":"0","recid":"2003269","relation_version_is_last":true,"title":["紀伊水道及びその外域における黒潮蛇行期と非蛇行期の平均水温について"],"weko_creator_id":"10","weko_shared_id":-1},"updated":"2025-04-17T08:37:32.359483+00:00"}