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Broadband sound propagation in shallow water and geoacoustic inversion

机译:浅水中的宽带声音传播和地声反演

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Part of an experiment to test a measurement package in a shallow water region in the Gulf of Mexico was designed to gater broadband acoustic data suitable for inversion to estimate seabed geoacoustic parameters. Continuous wave tow acoustic signals at multiple frequencies and broadband impulsive source signals were recorded on a horizontal line array in a high-noise environment. Simulated annealing with a normal mode forward propagation model is utilized to invert for a geoacoustic representation of the seabed. Several inversions are made from different data samples of two light bulb implosions, the measured sound speed profiles at the HLA and at the positions of the light bulb deployments, and for two different cost functions. The different cost functions, measured sound speed profiles, and measured time series result in different inverted geoacoustic profiles from which transmission loss is generated for comparison with measurements. On the basis of physical consistency and from the comparison of the transmission loss and time series, a best estimate geoacoustic profile is selected and compared to those obtained from previously reported inversions. Uncertainties in the sound speed profile are shown to affect the uncertainties of the estimated seabed parameters.
机译:在墨西哥湾的一个浅水区中测试测量包的实验的一部分,旨在对适合于反演的宽带声数据进行选通,以估算海床的地声参数。在高噪声环境中,将多个频率的连续波拖曳声信号和宽带脉冲源信号记录在水平线阵列上。利用正态正向传播模型进行的模拟退火可以反演海床的地声。根据两个灯泡内爆的不同数据样本,在HLA和灯泡部署位置处测得的声速曲线以及两个不同的成本函数,进行了几种反演。不同的成本函数,测得的声速剖面和测得的时间序列会导致不同的倒置地球声学剖面,从中会产生传输损耗以与测量结果进行比较。根据物理一致性,并根据传输损耗和时间序列的比较,选择最佳估计的地声剖面并将其与从先前报道的反演获得的地声剖面进行比较。声速剖面中的不确定性会影响估计海床参数的不确定性。

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