使用现实的大气和地形,对区域热层超声波的有限频建模
Jordan W Bishop1,2, Philip Blom2, David Fee1
1Wilson Alaska Technical Center, Geophysical Institute, University of Alaska Fairbanks, Fairbanks, Alaska 99709, USA.
The Journal of the Acoustical Society of America
|January 4, 2024
概括
有限频的超声波传播建模显示,现实的地形显著影响区域距离的波浪行为. 这种方法比传统的几何声学更好地解释观察到的信号,突出地形.
科学领域:
- 声学 声学 在声学方面
- 地质物理学 地质物理学
- 大气科学 大气科学
背景情况:
- 超声波通过热带层区域地传播.
- 几何声学模型的地形散射,但错过了有限频效应,如衍射.
- 射线方法在现实的大气条件下与复杂的波浪现象作斗争.
研究的目的:
- 开发和应用有限差异时间域 (FDTD) 方法来模拟超声波传播.
- 调查现实的地形和大气条件对超声波信号的影响.
- 将FDTD结果与几何声学预测进行比较.
主要方法:
- 开发了一种2D有限差异时间域 (FDTD) 方法,用于线性化的声波方程.
- 模拟了100公里的声波传播,横跨平坦和高斯山地形.
- 应用FDTD来模拟2012年犹他州测试和训练场地表面爆炸的超声波信号.
主要成果:
- 与射线预测不同的是,FDTD模拟准确地捕获了有限频传播效应.
- 包括地形和有限频率效应解释了来自犹他州爆炸的观察到的超声波信号.
- 模拟了通过热带层的传播,即使在弱管道条件下.
结论:
- 几何声学可能低估了热层的超声波传播.
- 现实的地形和有限频率效应对于理解区域性超声波波形至关重要.
- FDTD建模为超声波传播研究提供了更全面的方法.
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