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Hokkaido University Collection of Scholarly and Academic Papers >
Graduate School of Fisheries Sciences / Faculty of Fisheries Sciences >
北海道大学水産科学研究彙報 = Bulletin of Fisheries Sciences, Hokkaido University >
第58巻 第3号 >
2006年5月末の北海道亀田半島沖で発生した急潮現象
Title: | 2006年5月末の北海道亀田半島沖で発生した急潮現象 |
Other Titles: | The Kyucho occurred off Kameda Peninsula, Hokkaido, at the end of May, 2006 |
Authors: | 小林, 直人1 Browse this author | 磯田, 豊2 Browse this author →KAKEN DB | 小林, 雅行3 Browse this author | 佐藤, 千鶴4 Browse this author | 木村, 修5 Browse this author | 山口, 秀一6 Browse this author | 高津, 哲也7 Browse this author →KAKEN DB | ロザ, アナ ルイザ8 Browse this author |
Authors(alt): | Kobayashi, Naoto1 | Isoda, Yutaka2 | Kobayashi, Masayuki3 | Satoh, Chizuru4 | Kimura, Osamu5 | Yamaguchi, Hidekazu6 | Takatsu, Tetsuya7 | Rosa, Ana Luisa8 |
Keywords: | Kyucho | Kameda peninsula | halocline | rainfall water | wind-induced internal Kelvin wave |
Issue Date: | 28-Feb-2009 |
Publisher: | 北海道大学大学院水産科学研究院 |
Journal Title: | 北海道大学水産科学研究彙報 |
Journal Title(alt): | Bulletin of Fisheries Sciences, Hokkaido University |
Volume: | 58 |
Issue: | 3 |
Start Page: | 29 |
End Page: | 41 |
Abstract: | A large damage to fishing set-nets caused by the Kyucho occurred off Kameda peninsula on 30 May, 2006. Such Kyucho seldom occurs in this area and hence it is unusual phenomenon. Two current-meters setting off Usujiri located at Kameda peninsula and off Shiraoi faced the Hidaka Bay captured this sudden and swift current. The meteorological and oceanographical conditions in 2005 without the Kyucho and those in 2006 with the Kyucho were compared. The difference in both years was the oceanic stratification. That is, the surface halocline was thinly formed by a large quantity of rainfall water accompanied by the atmospheric disturbance on 28 May in 2006, before the Kyucho occurrence. In the case of such discontinuity subsurface thinner layer than usual, we will expect that the particle velocity of wind-induced internal Kelvin wave increases, but its phase propagation speed rather decreases. In fact, the observed surface current velocity (0.3-1.2 m/s) is almost as same as the estimated propagation speed (0.3-0.8 m/s). |
Type: | bulletin (article) |
URI: | http://hdl.handle.net/2115/36085 |
Appears in Collections: | 北海道大学水産科学研究彙報 = Bulletin of Fisheries Sciences, Hokkaido University > 第58巻 第3号
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