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Passive characterization of underwater acoustic waveguides through interferometry of diffuse ambient noise

机译:通过散射环境噪声的干涉法对水下声波导管进行无源表征

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It was recently demonstrated experimentally that sound-speed profiles in the ocean can be retrieved with oceanographically relevant accuracy from cross-correlation functions of ambient noise recorded on hydrophones separated by O(1)km. To be of practical interest, passive ocean acoustic tomography should work at ranges O(100)km or larger. An extension of passive tomography to such ranges requires retrieval of deterministic travel times or phases of normal modes from cross-correlation functions of imperfectly diffuse noise fields. Here we study diffuse noise fields generated by random sound sources distributed on a surface or in a volume in a horizontally-inhomogeneous waveguide. We show that two-point cross-correlation function of imperfectly diffuse noise field contains the same information about phases and travel times of adiabatic normal modes as would be obtained in a reciprocal transmission experiment, where each noise-recording hydrophone is replaced with an acoustic transceiver. Our theoretical results suggest using noise interferometry for passive acoustic characterization of ocean dynamics.
机译:最近通过实验证明,可以从与O(1)km分开的水听器上记录的环境噪声的互相关函数中,以海洋学相关的精度检索海洋中的声速剖面。为了实用,被动式海洋声层析成像应在O(100)km或更大的范围内工作。将被动层析成像技术扩展到这样的范围需要从不完全扩散的噪声场的互相关函数中获取确定的传播时间或正常模式的相位。在这里,我们研究由随机声源产生的扩散噪声场,这些声源分布在水平不均匀波导的表面或体积中。我们表明,不完全扩散噪声场的两点互相关函数包含与绝热法向模式的相位和传播时间相同的信息,这与在双向传输实验中获得的相同,在该实验中,每个噪声记录水听器都被声学收发器取代。我们的理论结果表明,将噪声干涉法用于海洋动力学的无源声学表征。

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