观察陆上直向向前的和在水中反向散射的波浪,它们在形海洋中传播
Xiaohan Wang1,2,3, Yang Dong1,2,3, Shengchun Piao1,2,3
1National Key Laboratory of Underwater Acoustic Technology, Harbin Engineering University, Harbin 150001, China.
JASA express letters
|May 8, 2025
概括
在形海洋中的低频声波根据频率表现不同. 高频分散,而低频作为地声波在岸上传播.
科学领域:
- 海洋声学 海洋声学
- 地震学 地震学
- 地质物理学 地质物理学
背景情况:
- 了解复杂的海洋环境中的声学传播至关重要.
- 海底地形显著影响声波的行为.
研究的目的:
- 在形海洋中研究低频声传播.
- 为了区分高频和低频声信号的传播机制.
主要方法:
- 部署海洋底地震计 (OBS) 和陆基地震计 (LS).
- 使用宽带声源 (空气枪).
- 用光谱元素建模来分析波传播.
主要成果:
- OBS记录了前向直流和后向分散的波.
- LS检测到与岸相连的直向到达.
- 频率依赖的传播:>200Hz分散,<200Hz合到海底.
结论:
- 在形海洋中的声学传播是频率依赖的.
- 低频声波 (<200 Hz) 可以在海底结合,并在陆上以地声波的形式传播.
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