摘要
本文采用已建立厦门港潮流场、盐度场和水质点拉格朗日运动的模型。模拟了盐度场分布和漂流浮子的运动轨迹，与现场盐度调查和浮子跟踪试验结果基本一致，分析厦门港河口区“退潮流隔”形成的动力机制。佐证“退潮流隔”是河口区咸淡水相互作用的“退潮锋面”形成的主要动力机制。
The tidal current simulation in Xiamen Harbour is present. Especially a Lagrangian model of water point movement is given. Based on drift tracking and ordinary daily salt measurement, the bony movement trace and the salt distribution is simulated. Dynamic mechanisms of the ebb front in Xiamen Harbour is analyzed. It is shown that there is a ebb current partition in Jiulongjiang Estuary.
出处
《台湾海峡》
CAS
CSCD
1999年第4期437-444,共8页
Journal of Oceanography In Taiwan Strait
基金
国家自然科学基金!49476290
