在海底山脉附近的深水中模拟和解释双静态底部反响
Yue Guo1, Rui Duan1, Hao Zhang1
1School of Marine Science and Technology, Northwestern Polytechnical University, Xi'an, Shaanxi 710072, China.
The Journal of the Acoustical Society of America
|November 16, 2023
概括
研究人员使用一种新的模型解释了深海反响数据中的不同寻常的明亮条纹. 这个模型与方程系统相结合,准确地复制和解释了海底山脉的散射,增强了我们对水下声学的理解.
科学领域:
- 海洋声学 海洋声学
- 地物理信号处理的信号处理.
背景情况:
- 深海的反响是复杂的,因为多路径的传播,特别是海底的不同地形.
- 垂直阵列生成垂直角度时间记录 (VATR) 用于分析时空特征.
- 在一项与海平面散射相关的双静态反响实验中,在VATR中观察到奇特的明亮条纹.
研究的目的:
- 开发一个模型来复制和解释VATR中观察到的明亮条纹.
- 量化地将海平面参数与观察到的条纹结构联系起来.
- 为深海反响中的异常条纹现象提供全面的解释.
主要方法:
- 建立了一个比斯塔斯反响模型来复制VATR并模拟时空反响.
- 引入了一个方程系统,以基于海底层参数计算条纹参数.
- 分析了条纹特征对海底特征的依赖性.
主要成果:
- 双声波声模型有质地解释了观察到的明亮条纹.
- 方程系统使得基于海底层几何学的条纹结构的定量预测成为可能.
- 结合的模型和方程成功地复制和解释了实验观察结果.
结论:
- 开发的模型和方程系统为了解深海反响中海拔引起的散射提供了一个强大的框架.
- 这项工作增强了在地质上多样化的水下环境中复杂声学信号的解释.
- 对这些现象的准确建模对于声纳性能和水下探索至关重要.
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