Department of Naval Architecture and Ocean Engineering, Chonnam National University, Yeosu, Jeollanam-do 550-749, Republic of Korea.
Mar Environ Res. 2010 Aug;70(2):227-38. doi: 10.1016/j.marenvres.2010.05.005. Epub 2010 May 19.
We conducted field observations to investigate the cause of Cochlodinium polykrikoides blooms in the Korean Southern Coastal Waters (KSCW), and also analyzed information on marine environmental factors obtained from the National Fisheries and Development Institute (NFRDI), from 1995 to 2008. Long-term tidal currents revealed a two-layered flow with the upper current flowing toward Boddolbada located between Narodo and Nammyeon, and the lower current out of the bay. Water temperatures were higher at the north than at the south of the bay, whereas salinities exhibited the reverse trend. C. polykrikoides blooms occurred at a water temperature of approximately 25.0-26.0 degrees C and a salinity of approximately 31.00 in the seas neighboring Narodo Islands. The outbreak of C. polykrikoides blooms in the seas neighboring Narodo Islands in summer was influenced by thermohaline fronts observed between the KSCW and Tsushima Warm Current (TWC).
我们进行了实地观测,以调查在韩国南部沿海水域(KSCW)中 Cochlodinium polykrikoides 水华爆发的原因,并分析了从 1995 年到 2008 年从国家渔业和发展研究所(NFRDI)获得的海洋环境因素信息。长期的潮流显示出两层流,上层水流向 Narodo 和 Nammyeon 之间的 Boddolbada,下层水流出海湾。湾内北部的水温高于南部,而盐度则相反。在邻近 Narodo 群岛的海域,当水温约为 25.0-26.0°C 且盐度约为 31.00 时,会发生 Cochlodinium polykrikoides 水华爆发。夏季邻近 Narodo 群岛海域 Cochlodinium polykrikoides 水华的爆发受到在 KSCW 和对马暖流(TWC)之间观察到的温盐锋的影响。