Ocean College, Zhejiang University, Zhoushan 316021, China.
National Innovation Institute of Defense Technology, Fengtai District, Beijing 100071, China.
Sensors (Basel). 2020 Aug 12;20(16):4498. doi: 10.3390/s20164498.
Coastal acoustic tomography (CAT), as an innovative technology, can perform water temperature measurements both in horizontal and vertical slices. Investigations on vertical slice observations are significantly fewer in number than horizontal observations due to difficulties in multi-path arrival peak identification. In this study, a two-station sound transmission experiment is carried out in Thousand-Island Lake, Hangzhou, China, to acquire acoustic data for water temperature profiling. Time windows, determined by range-independent ray simulation, are used to identify multi-path arrival peaks and obtain corresponding sound wave travel times. Special attention is paid to travel time correction, whose errors are caused by position drifting by more than 2 m of moored stations. The sound speed and temperature profiling are divided into four layers and are calculated by regularized inversion. Results show a good consistency with conductivity-temperature-depth (CTD) measurements. The root mean square error (RMSE) of water temperature is 0.3494, 0.6838, 1.0236 and 1.0985 °C for layer 1, 2, 3 and 4, respectively. The fluctuations of measurement are further smoothed by the moving average, which decreases the RMSE of water temperature to 0.2858, 0.4742, 0.7719 and 0.9945 °C, respectively. This study illustrates the feasibility and high accuracy of the coastal acoustic tomography method in short-range water temperature measurement. Furthermore, 3D water temperature field profiling can be performed with combined analyzing in horizontal and vertical slices.
沿海声层析成像(CAT)作为一种创新技术,可以在水平和垂直切片中进行水温测量。由于多径到达峰识别困难,垂直切片观测的研究数量明显少于水平观测。本研究在中国杭州千岛湖进行了两站声传播实验,以获取水温剖面的水声数据。通过无距离射线模拟确定的时窗用于识别多径到达峰并获得相应的声波传播时间。特别注意传播时间修正,其误差是由停泊站位置漂移超过 2 米引起的。声速和温度剖面分为四层,并通过正则化反演进行计算。结果与电导率-温度-深度(CTD)测量具有很好的一致性。第 1、2、3 和 4 层的水温均方根误差(RMSE)分别为 0.3494、0.6838、1.0236 和 1.0985°C。通过移动平均进一步平滑测量值的波动,将水温的 RMSE 分别降低到 0.2858、0.4742、0.7719 和 0.9945°C。本研究说明了沿海声层析成像方法在短距离水温测量中的可行性和高精度。此外,还可以通过水平和垂直切片的联合分析来进行 3D 水温场剖面测量。