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根据多途结构到达时间间隔大小与温跃层水文环境参数之间的关系 ,研究利用多途结构的变化来监测由内波 (或内潮汐 )引起的温跃层起伏的方法。并从实验上验证了这一方法的可行性
According to the relationship between the multi-way structure arrival time and the parameters of the thermocline hydrological environment, the method of monitoring the thermocline fluctuation caused by the inner wave (or the inner tide) by using the changes of the multi-way structure is studied. The feasibility of this method is verified experimentally