观测和建模的三维声传播沿着一个非线性内部引力波在架间破裂的观察和建模
Tzu-Ting Chen1, Ying-Tsong Lin2, Linus Y-S Chiu3
1Institute of Oceanography, National Taiwan University No.1, Sec. 4, Roosevelt Road, Taipei, Taiwan.
The Journal of the Acoustical Society of America
|February 6, 2025
概括
非线性内部重力波 (NIW) 和海底斜率对水下声学产生重大影响. 它们的综合效果,特别是3D声道,可以在4.8公里内将声强度提高到9.5dB.
科学领域:
- 海洋声学 海洋声学
- 水下声音传播的传播方式
- 地质物理流体动力学
背景情况:
- 水下声音传播受到内部波浪和海底地形等环境因素的影响.
- 非线性内部重力波 (NIWs) 产生强烈的声速梯度.
- 海底的斜率会影响声学反射方向.
研究的目的:
- 为了研究NIW和海底斜率的联合声学效应.
- 为了分析来自南中国海架裂的实验数据.
- 为了比较2D和3D声音传播模型.
主要方法:
- 来自水音机垂直线阵列的实验数据的分析.
- 使用2D和3D数值声音传播模型.
- 射线追踪路径和传输损失的比较.
主要成果:
- 由于NIW和海底斜率而观察到的声信号变化.
- 3D声传播模型显示了显著的声强度增加.
- 在NIW前线和海底斜坡之间的3D音频管道在4.8公里内引起了高达9.5dB的强度增加.
结论:
- NIW和海底斜率共同影响水下声学信号.
- 在这样的环境中,为准确建模声音传播,3D 效果至关重要.
- 声导体现象可以导致声强度大幅增加.
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