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Estimation of stability of acoustic reciprocal transmission in deep and coastal waters

机译:估计深水和沿海水域的声波相互传播的稳定性

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摘要

Ocean acoustic tomography (OAT) is a powerful approach for observation of deep and coastal water fluctuations. A precise estimation of travel time is essential for measuring ocean current using OAT. Generally, sound waveforms on reciprocal propagation that are transmitted at the same time are similar mutually, and it is considered that their correlation is high. However, we found that reciprocal sound waveforms sometimes become different in the continuous estimation of travel time difference. In this paper, we present the estimation results of the correlation between the reciprocal transmissions. We estimate the variation of the correlation of reciprocal propagated sound transmissions. Alow correlation between the reciprocal propagated sound waveforms occurs at a certain rate on long range propagation in deep ocean. Acoustic measurement accuracy of current velocity in deep and coastal water is also estimated.
机译:海洋声学层析成像(OAT)是观察深水和沿海水域波动的有力方法。对于使用OAT测量洋流,准确估计行进时间至关重要。通常,同时传播的相互传播的声音波形彼此相似,可以认为它们的相关性很高。但是,我们发现,在连续估计行进时间差时,相互的声音波形有时会变得不同。在本文中,我们介绍了相互传递之间的相关性的估计结果。我们估计相互传播的声音传输的相关性的变化。在深海的远距离传播中,相互传播的声波波形之间的低相关性以一定的速率发生。还估算了深水和沿海水域中流速的声学测量精度。

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