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作 者:张学庆[1] 孙雅杰 王兴[1] 刘培廷[2] 熊瑛[2]
机构地区:[1]中国海洋大学环境科学与工程学院,山东青岛266100 [2]江苏省海洋水产研究所,江苏南通226007
出 处:《海洋环境科学》2017年第3期427-433,共7页Marine Environmental Science
基 金:江苏省科技基础设施建设计划(BM2012059);国家重点基础研究发展计划项目(973计划)(2015CB453301)
摘 要:基于Environment Fluid Dynamic Code(EFDC)模型,利用水龄概念,研究潮和风对海州湾及毗邻海域水交换的影响。结果表明,全年统计风场下,海州湾的平均水龄相对纯潮流作用下变化幅度为-48.5%~18.4%;夏季风场有利于海州湾的水体交换,水交换时间比纯潮流作用下减小36.3%;冬季风场会减缓海州湾的水体交换,水交换时间比纯潮流作用下增加40.8%,研究表明在开阔海域,季风对水交换影响显著,水交换的季节变化很好地解释了海州湾近岸冬季污染物浓度高、夏季污染物浓度低的动力机制。Based on Environment Fluid Dynamic Code( EFDC) Model,the concept of water age is used to study the effect of tide and wind on the water exchange time in Haizhou bay and adjacent regions. The results show that the range of the average water age is-48. 5% - 18. 4% under annual statistics wind. The summer wind is in favor of the water exchange,and the water exchange time under summer wind conditions is 36. 3% less than that under the tidal force condition only. However,the winter wind slows down the water exchange,and the water exchange time under winter wind conditions can be 40. 8% more than that under the tidal force condition only. The study shows that the water exchange in open sea area is significantly affected by the monsoon,and the seasonal changes of the water exchange well explain the dynamic mechanism of the seasonal changes of the pollutant distribution.
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