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Pekeris声波导情况下海深不确定性对简正波群速度反演海底声速的影响研究

The influence of the uncertainty of water depth on the inversion of bottom sound speed based on normal mode group velocities in Pekeris waveguides

  • 摘要: 简正波群速度广泛应用于海底参数反演,海深不确定性对反演结果有较大影响。为了减小海深测量误差对反演结果的影响,本文通过理论分析和仿真计算对Pekeris声波导情况下正则简正波群速度随海深和海底声速的变化规律进行研究,结果表明当所选取的频率处于某号简正波的Airy频率附近时,该号简正波的群速度对海深变化不敏感,而比同频率的低号简正波的群速度受海底声速的影响更大。将这一变化规律应用于由简正波群速度反演海底声速,仿真与实验结果表明,应用Airy频率附近的简正波的群速度反演海底声速,能有效克服海深不确定性对反演结果的影响。

     

    Abstract: The group velocities of normal modes are widely used in geo-acoustic inversion, and the uncertainty of water depth affects the inversion results. In order to reduce this effect, the law of normal modes' group velocities in Pekeris waveguides versus the water depth and the bottom sound speed is studied in this paper. It is shown that if the frequency is around the Airy frequency of a normal mode, the group velocity of the normal mode is not sensitive to the water depth. But the bottom sound speed has greater influence on the group velocity of that normal mode than the group velocities of lower modes at the same frequency. The group velocities of normal modes are applied to the inversion of the bottom sound speed. The numerical and experimental results show that the influence of the uncertainty of water depth on the inversion results is significantly reduced if the normal modes whose associated Airy frequencies are near the working frequency.

     

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