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理论和数值研究的短暂的声波传播穿过冰层在北冰洋的冰层
Qitian Zeng1, Shengxing Liu1,2, Liguo Tang1,3
1Key Laboratory of Underwater Acoustic Communication and Marine Information Technology (Ministry of Education), College of Ocean and Earth Sciences, Xiamen University, Xiamen 361102, China.
The Journal of the Acoustical Society of America
|May 10, 2024
概括
在北极冰层中短暂的声波传播被研究为跨冰通信. 较厚的冰和较长的距离导致更大的波形扭曲,影响系统设计.
科学领域:
- 地质物理学 地质物理学
- 声学 声学 在声学上
- 海洋学 海洋学 海洋学
背景情况:
- 北冰洋冰层对声波传播提出了独特的挑战.
- 了解短暂的声学行为对于开发有效的跨冰通信系统至关重要.
研究的目的:
- 从理论上分析穿过北冰洋冰层的短暂声波传播.
- 为设计可靠的声音通信系统提供指导,这些系统可以穿透冰.
主要方法:
- 模拟了北冰洋作为一个复合的冰水结构.
- 处理冰作为弹性固体和水作为液体.
- 通过自函数扩展方法推导出一种分析的短暂解.
- 采用数值程序来分析声波特征.
主要成果:
- 辐射位移的波形显示出比轴向位移更严重的扭曲.
- 辐射和轴移幅都随着传播距离的增加而迅速减少.
- 冰的厚度显著影响了辐射位移,而不是轴向位移,随着厚度的增加,扭曲也会增加.
结论:
- 波形扭曲和振幅衰减是跨冰声通信的关键因素.
- 冰厚是影响信号完整性和通信系统设计的关键参数.
- 这些发现为优化在冰冷环境中的声通信提供了理论见解.
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