Factors controlling the spatio-temporal distribution of the 2009 Chattonella antiqua bloom in the Yatsushiro Sea, Japan

被引:18
|
作者
Aoki, Kazuhiro [1 ]
Onitsuka, Goh [2 ]
Shimizu, Manabu [1 ]
Kuroda, Hiroshi [3 ]
Matsuyama, Yukihiko [4 ]
Kimoto, Katsunori [4 ]
Matsuo, Hitoshi [5 ]
Kitadai, Yuuki [5 ]
Sakurada, Kiyonari [6 ]
Nishi, Hiromi [7 ]
Tahara, Yoshio [7 ]
机构
[1] Fisheries Res Agcy, Natl Res Inst Fisheries Sci, Kanazawa Ku, Yokohama, Kanagawa 2368648, Japan
[2] Fisheries Res Agcy, Natl Res Inst Fisheries & Environm Inland Sea, Hiroshima 7390452, Japan
[3] Fisheries Res Agcy, Hokkaido Natl Fisheries Res Inst, Kushiro 0850802, Japan
[4] Fisheries Res Agcy, Seikai Natl Fisheries Res Inst, Nagasaki 8512213, Japan
[5] Azuma Cho Fishery Cooperat Assoc, Nagashima, Kagoshima 8991401, Japan
[6] Kumamoto Prefectural Fisheries Res Ctr, Kumamoto 8693603, Japan
[7] Kagoshima Prefectural Fisheries Technol & Dev Ctr, Ibusuki, Kagoshima 8910315, Japan
关键词
Chattonella antiqua; Lagrangian simulation; current transport; river flushing; northeasterly wind; Japan; Yatsushiro Sea; MARINA RAPHIDOPHYCEAE; DYNAMICS; GROWTH; TEMPERATURE; IRRADIANCE; SALINITY; MODEL; ALGA;
D O I
10.1016/j.ecss.2012.08.028
中图分类号
Q17 [水生生物学];
学科分类号
071004 ;
摘要
A harmful bloom due to the raphidophycean flagellate, Chattonella antiqua, was found in the Yatsushiro Sea, western Kyushu, Japan, from the end of July to the beginning of August 2009. The bloom resulted in enormous economic damage to cultured finfish production in aquaculture farms concentrated in the southwestern area. To investigate the factors controlling the spatio-temporal distribution of the bloom, data analysis and numerical simulations were conducted using field monitoring data and a three-dimensional hydrodynamic model coupled to a Lagrangian particle-tracking model. Results of the monitoring data analysis showed that the initial development of the C. antiqua bloom occurred in Kusuura Bay and the northeastern area near the mouth of the Kuma River, and subsequently the bloom expanded rapidly to the whole area. The simulation results indicated that the source region of the widespread bloom was not Kusuura Bay but the northeastern area. The southwestward evolution of the bloom was primarily controlled by the passive transport due to the surface residual current driven by fresh water discharge from the Kuma River and northeasterly winds. On the favorable conditions of river discharge and wind, the massive bloom of C. antiqua that formed in the northeastern area was quickly transported southwestward within a few days. (C) 2012 Elsevier Ltd. All rights reserved.
引用
收藏
页码:148 / 155
页数:8
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