{"created":"2024-04-25T05:05:37.107599+00:00","id":2003264,"links":{},"metadata":{"_buckets":{"deposit":"973a9680-ef53-461c-8302-3da141adba16"},"_deposit":{"created_by":10,"id":"2003264","owners":[10],"pid":{"revision_id":0,"type":"depid","value":"2003264"},"status":"published"},"_oai":{"id":"oai:fra.repo.nii.ac.jp:02003264","sets":["12:14:1716951205920"]},"author_link":["3356","3339","3337","1901"],"control_number":"2003264","item_10002_biblio_info_7":{"attribute_name":"bibliographic_information","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1985-10","bibliographicIssueDateType":"Issued"},"bibliographicNumberOfPages":"11","bibliographicPageEnd":"109","bibliographicPageStart":"99","bibliographicVolumeNumber":"19","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 fluctuations of stream axes of the Kuroshio Southwest of Japan, represented by Northwest off Naha, True South off Yakushima Island, Southeast off Cape Toi, True South off Capes Ashizurimisaki, Murotomisaki, Shionomisaki and Daiozaki, were described from the point of the presence or absence of the Kuroshio Meander off Enshunada South of Japan on the basis of the monthly oceanographic atlas reduced in our laboratory since 1968. During the Kuroshio with no Meander, the stream axes of the Kuroshio Southwest off Japan generally lie in the near shore. On the contrary, during the Kuroshio with Meander, the stream axes along the offing between Capes Ashizurimisaki and Shionomisaki show locally systematic offshore and inshore fluctuations together with the generation, cont inuance and disappearance of the Meander South of Japan. By the way, during the Kuroshio with no Meander, the stream axes Southwest of Japan sometimes change their flows in drastic manner accompanying with moderately large meanders. Some of them propagate downstream and act as a \"trigger\" for the Meander South of Japan. On the other hand, the downstream propagations of the meander to the East of Cape Shionomisaki during the Meander seem to have close relation to maintain the Meander South of Japan. It is remarkable from physical oceanographic standpoint that the same downstream phenomena seem to occur in the East China Sea and in the Southern Sea off Kyushu.","subitem_description_language":"en","subitem_description_type":"Abstract"},{"subitem_description":"1968年以降,月別に作成している海況図から得られた黒潮主軸資料を用いて,東シナ海をも含めた南西海域の代表的な岬,那覇北西,屋久島正南,都井岬南東,足摺岬正南,室戸岬正南,潮岬正南及び大王埼正南沖毎に主軸変動の特徴を,大蛇行の有無や海況の転換期に注目して記述した。足摺鉀正南沖から潮岬正南沖にいたる海域では,大蛇行,準大蛇行の発生,持続,消滅に伴って,黒潮主軸が,系統的でしかも局地性の強い離接岸変動を示すことを明らかにした。また,比較的変動が少ないといわれている南西海域の黒潮も,時には顕著な変動を示す。そして,非蛇行期においては,そのうちのいくつかが潮岬以東の海域にも波及し,大蛇行や準大蛇行の引き金となり,また,大蛇行期には,同様な現象が,大蛇行の持続に重要な働きをしていることを推察した。なお,那覇北西及び屋久島正南では,都井岬沖以東の黒潮変動に直接結びつくと思われる蛇行現象が見いだされており,黒潮流路予測研究のためにも,今後この海域に注目した調査·研究を進めていくことが重要である。","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 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