Huang Chen-Fen, Li Yun-Wen, Taniguchi Naokazu
Institute of Oceanography, National Taiwan University, No. 1, Sec. 4, Roosevelt Road, Taipei 10617, Taiwan.
J Acoust Soc Am. 2019 Feb;145(2):858. doi: 10.1121/1.5090496.
This study investigates techniques for the acoustic mapping of ocean currents in a shallow-water environment using moored and ship-towed stations. The currents are estimated using the differential travel times (DTTs) observed in the reciprocal acoustic transmissions between those stations. Due to the relative motion induced by the ship-towed station, the Doppler shift estimated from the measured channel impulse response is used to compensate for the arrival patterns and to correct the influence of the relative speed on the DTTs. Furthermore, to estimate the DTTs from the arrival patterns received in the reciprocal directions, a method is devised which involves the time-evolving cross-correlation function of the reciprocal arrival patterns. A feasibility test was carried out at Sizhiwan Marine Test Field, Kaohsiung, Taiwan in September of 2015. The currents were estimated using the data collected from one ship-towed and four moored stations. The estimated currents are consistent with the direct measurements from a shipboard acoustic Doppler current profiler and reveal the spatial distribution of the currents.
本研究调查了利用系泊站和船拖式站在浅水环境中进行洋流声学测绘的技术。利用在这些站点之间的双向声学传输中观测到的差分传播时间(DTT)来估计洋流。由于船拖式站引起的相对运动,从测量的信道脉冲响应估计的多普勒频移用于补偿到达模式,并校正相对速度对DTT的影响。此外,为了从双向接收的到达模式中估计DTT,设计了一种方法,该方法涉及双向到达模式的时间演化互相关函数。2015年9月在台湾高雄的四治湾海洋试验场进行了可行性测试。利用从一个船拖式站和四个系泊站收集的数据估计了洋流。估计的洋流与船上声学多普勒流速剖面仪的直接测量结果一致,并揭示了洋流的空间分布。