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東シナ海における黒潮の数日間の変化
http://hdl.handle.net/10232/683
http://hdl.handle.net/10232/683699beaa9-1fb1-44b1-8d64-32efaf883d8a
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
KJ00004175508.pdf (895.9 kB)
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| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
|---|---|---|---|---|---|---|
| 公開日 | 2015-04-20 | |||||
| タイトル | ||||||
| タイトル | 東シナ海における黒潮の数日間の変化 | |||||
| タイトル言語 | ja | |||||
| タイトル | ||||||
| タイトル | Temporal Change of the Kuroshio in the East China Sea During Several Days | |||||
| タイトル言語 | en | |||||
| 著者 |
中村, 啓彦
× 中村, 啓彦× 市川, 洋× 茶圓, 正明× 嶋田, 起宜× 内山, 正樹× 吉永, 圭輔 |
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| 言語 | ||||||
| 言語 | eng | |||||
| キーワード | ||||||
| 主題言語 | en | |||||
| 主題Scheme | Other | |||||
| 主題 | The Kuroshio axis | |||||
| キーワード | ||||||
| 主題言語 | en | |||||
| 主題Scheme | Other | |||||
| 主題 | The Kuroshio front | |||||
| キーワード | ||||||
| 主題言語 | en | |||||
| 主題Scheme | Other | |||||
| 主題 | Temporal change | |||||
| 資源タイプ | ||||||
| 資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
| 資源タイプ | departmental bulletin paper | |||||
| アクセス権 | ||||||
| アクセス権 | open access | |||||
| アクセス権URI | http://purl.org/coar/access_right/c_abf2 | |||||
| 要約 | ||||||
| 内容記述タイプ | Other | |||||
| 内容記述 | In order to examine temporal changes of the Kuroshio, the observation was carried out twice on March 1-4 and March 7-10, 1997 along three sections across the Kuroshio in the East China Sea by T/V Keitenmaru of Kagoshima University. Two of these sections were located in the continental slope region and one in the Tokara Strait. Horizontal shifts of the surface temperature front (hereafter, called the Kuroshio front) were closely related to those of the position of the maximum surface velocity (hereafter, called the Kuroshio axis) in all cross-sections. However, the former varied with a several times (1.8～7) larger amplitude than the latter. The Kuroshio in the Tokara Strait was focused on, because the Kuroshio axis shifted northward with the large distance of 60km during 8 days. The vertical structure of the Kuroshio in the strait was characterized by the upper- and lower-interfaces. The maximum tilt of the lower-interface geographically corresponded to the Kuroshio axis. On the other hand, the outcropping of the upper-interface corresponded to the Kuroshio front. Since the structure of the lower-interface changed little during the northward migration of the Kuroshio, the surface velocity at the Kuroshio axis was maintained. The structure of the upper-interface changed significantly, and this resulted in the horizontal shift of the Kuroshio front with a twice larger amplitude than the Kuroshio axis. These observations suggest that the fluctuation of the Kuroshio axis is dynamically different from that of the Kuroshio front. | |||||
| 内容記述言語 | en | |||||
| 収録雑誌名 |
ja : 鹿児島大学水産学部紀要 en : Memoirs of Faculty of Fisheries Kagoshima University 巻 46, p. 11-20, 発行日 1997-12-24 |
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| 作成日 | ||||||
| 日付 | 1997-12-24 | |||||
| 日付タイプ | Issued | |||||
| ISSN | ||||||
| 収録物識別子タイプ | PISSN | |||||
| ISSN | 0453087X | |||||
| NII書誌ID（雑誌） | ||||||
| 収録物識別子タイプ | NCID | |||||
| NC ID | AN00040498 | |||||
| 出版タイプ | ||||||
| 出版タイプ | VoR | |||||
| 出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||
| NDC | ||||||
| 主題Scheme | NDC | |||||
| 主題 | 660 | |||||
| NIIsubject | ||||||
| 主題言語 | ja | |||||
| 主題Scheme | Other | |||||
| 主題 | 自然科学 | |||||
| 公開者・出版者 | ||||||
| 出版者 | 鹿児島大学 | |||||
| 出版者言語 | ja | |||||
| 公開者・出版者 | ||||||
| 出版者 | Kagoshima University | |||||
| 出版者言語 | en | |||||
