2016年10月
Numerical study for specifying the major origin of low salinity water associated with Chattonella (Raphidophyceae) blooms in Tachibana Bay, Japan
JOURNAL OF OCEANOGRAPHY
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- 巻
- 72
- 号
- 5
- 開始ページ
- 811
- 終了ページ
- 816
- 記述言語
- 英語
- 掲載種別
- 研究論文(学術雑誌)
- DOI
- 10.1007/s10872-016-0376-y
- 出版者・発行元
- SPRINGER
In both 2009 and 2010, massive Chattonella blooms occurred in Tachibana Bay. Observation results show that high cell densities of Chattonella were distributed in the central area of Tachibana Bay with low salinity water. Model results indicate that the low salinity water originated from the Ariake Sea and intruded into Tachibana Bay during the northerly or weak winds. It is suggested that low salinity water was mainly discharged from the northern area of the Ariake Sea. Northerly wind enhanced the horizontal advection of the low salinity water intruding into Tachibana Bay originating from the northern area of the Ariake Sea.
- リンク情報
- ID情報
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- DOI : 10.1007/s10872-016-0376-y
- ISSN : 0916-8370
- eISSN : 1573-868X
- Web of Science ID : WOS:000384532600012