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Observations on fluctuations of sound transmission and temperature field from the ASIAEX 2001 South China Sea experiment and inversion of the characterizations of internal tides (waves)

机译:从ASIAEX 2001南海实验观察到的声波传播和温度场的波动以及内潮(波)的特征反演

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摘要

Two conclusions are obtained by analyzing the fluctuation data of the temperature field and the sound transmission in the South China Sea from ASIAEX 2001 volume interaction experiment. First of all, the peak-to-peak value of the particle vertical mean displacement due to the internal waves exceeds 40 m. Secondly, the peak-to-peak value of the sound transmission fluctuations represented by the pulse leading-edge fluctuations of the travel-time average exceeds 100 ms. Based on that, the major components of the internal waves are obtained by analyzing the spectrum of the temperature field fluctuations. The spectrum structures of the temperature field fluctuations in the across-shelf and the along-shore directions are compared respectively, and the spectrum structures of the sound transmission in such two different directions are also compared. The multi-path signals and the travel-time of the pulse are respectively used to capture the information of the sound transmission fluctuations, and their spectrum structures are compared also.
机译:通过分析ASIAEX 2001体积相互作用实验对南海温度场和声传播的波动数据,得出两个结论。首先,由内部波引起的粒子垂直平均位移的峰峰值超过40 m。其次,由传播时间平均值的脉冲前沿波动表示的声音传递波动的峰峰值超过100ms。在此基础上,通过分析温度场涨落的频谱来获得内部波的主要成分。分别比较了跨架方向和沿岸方向的温度场涨落的频谱结构,并且还比较了沿这两个不同方向的声音传输的频谱结构。多径信号和脉冲的传播时间分别用于捕获声音传输波动的信息,并对它们的频谱结构进行比较。

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