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在波福特海中观察到的传输和海洋冰声学合建模
David R Barclay1, Bruce S Martin2, Paul C Hines3
1Department of Oceanography, Dalhousie University, 1355 Oxford Street, Halifax, Nova Scotia B3H 4R2, Canada.
The Journal of the Acoustical Society of America
|July 5, 2023
概括
一个新的合海洋冰声学模型准确地模拟了波福特海的声音传播. 该模型捕捉了声损失的季节性变化,验证了其对北极声学研究的有效性.
科学领域:
- 海洋学 海洋学 海洋学
- 声学 声学 在声学方面
- 海冰物理学 海洋冰物理学
背景情况:
- 在动态的北极环境中,准确的声传播建模至关重要.
- 以前的模型缺乏对冰盖特征及其对声音的影响的详细表示.
研究的目的:
- 为波福特海开发和验证一个结合的海洋-冰-声学模型.
- 评估模型能够复制观测到的声学传播损失的能力.
主要方法:
- 通过使用全球预报数据,配置了一个合的海洋冰声学模型.
- 采用双模粗度算法来实现现实的冰盖生成.
- 将冰的特性和声速配置文件集成到一个抛物线方程声学模型中.
主要成果:
- 模型生成的冰盖统计数据与观察数据保持一致.
- 预测的声学接收级别与一年的测量 (35 Hz 和 925 Hz) 有合理的一致性.
- 传播损失的季节性和次季节性变化在925Hz时被准确地复制.
结论:
- 结合模型为北极声传播研究提供了一个强大的工具.
- 该模型成功地捕捉了冰洋动态对声音传输的影响.
- 经过验证的模型性能支持其用于理解北极声学环境.
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