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Sound Propagation in Deep Water with the Presence of Seamounts

机译:在深水中具有Seamounts的声音传播

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Seamounts in deep water have significant effects on the sound propagation. However, the reconstruction of the broadband pulses behind a seamount is indeed challenging due to the complex environment. It seems worthy to investigate the effects of seamounts on sound propagation in deep water. An experiment was conducted in 2014 in the Southern China Sea to investigate sound propagation in an environment with and without seamounts. The effects of seamounts on sound propagation were analyzed by using the broadband signals from the two propagation tracks. Transmission losses (TLs) differences for propagation in the environments with and without seamount are observed. When seamount located in the first shadow zone, the TLs decrease up to 7 dB before the seamount due to reflection of the bathymetry. The convergence zone structures are destroyed by the direct blockage of seamount and TLs increase more than 30 dB behind the seamount. Abnormal TLs and pulse arrival structures are explained by using ray theory. The numerical TLs and pulse arrival structures can match with experimental results.
机译:深水中的海山对声音传播产生了显着影响。然而,由于复杂的环境,海山背后的宽带脉冲的重建确实具有挑战性。探索海山对深水中声音传播的影响似乎值得。在2014年在南方海洋中进行了一个实验,以调查有和没有海山的环境中的声音传播。通过使用来自两个传播轨道的宽带信号分析了Seamounts对声音传播的影响。观察到在有和没有Seamount的环境中传播的传输损耗(TLS)差异。当Seamount位于第一阴影区中时,由于浴约定的反射,TLS在海山之前高达7dB。收敛区结构被Seamount的直接堵塞破坏,并且TLS增加了超过30dB的海山后面。通过使用光线理论来解释异常的TLS和脉冲到达结构。数值TLS和脉冲到达结构可以与实验结果相匹配。

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