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Influences of wind field on flow regime and algae blooming in Dianshan Lake

机译:风野对滇山流动制度与藻类的影响

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Wind rose analysis method, two dimensional hydrodynamic model and particle tracer model are adopted to systematically study wind field features, flow field variation, and migration, spreading and accumulation processes of the internal and external cyanobacterial boom in Dianshan Lake. The results show that the wind direction in Dianshan Lake varies with seasons; the main wind direction is ESE in summer and autumn, and is NNW in winter and spring. Wind has great effects on the circulation patterns of the lake. In the case of no wind, the lake is mainly influenced by the upstream and downstream flows. River flow enters into the lake during flood tide, while the lake discharges during ebb tide, and there is no circulation occurred; the clockwise and counterclockwise circulations are generated respectively in the north and south of the lake under southeast wind, and similarly for northwest wind only the circulation directions are opposite. Upon different wind and flow fields, cyanobacterial boom is drifting to the windward lakeshore, and is prone to form the algae accumulation area.
机译:玫瑰风分析方法,二维流体力学模型和颗粒示踪模型采用有系统地研究风场特征,流场的变化,和迁移,扩散和淀山湖内部和外部蓝藻吊杆的累积过程。结果表明,在淀山湖风向随季节变化而变化;主要风向为夏季和秋季ESE,是北北西在冬季和春季。风已经在湖的流通模式有很大影响。在无风的情况下,湖水主要由上游和下游流动的影响。河流进入涨潮时期的湖泊,而退潮时期的湖泊排放,并没有发生循环;顺时针和逆时针环流在湖的东南风下的北部和南部分别产生,同样为西北风只流通方向相反。在不同的风力和流场,蓝藻吊杆漂流到迎风湖岸,并且是易于形成的藻类堆积区域。

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