北大西洋上海声音通道的变化
Gregg A Jacobs1, Robert W Helber1, John M Toole2
1Naval Research Laboratory, Stennis Space Center, Mississippi 39529, USA.
The Journal of the Acoustical Society of America
|June 23, 2025
概括
北大西洋的声音通道与特定的水体和位置有关. 改进的海洋模型更好地代表了这些声音通道及其相关的水特性.
科学领域:
- 海洋学 海洋学 海洋学
- 声学 声学 在声学方面
- 数字建模 数字建模
背景情况:
- 声音通道对于水下声学至关重要,并受海洋学条件的影响.
- 了解声音通道分布有助于评估数值海洋模型的性能.
- 以前的研究已经描述了一般的声音通道行为,但需要详细的区域分析.
研究的目的:
- 描述北大西洋的声音通道分布.
- 研究声道与水体之间的关系.
- 评估数值海洋模型在模拟声音通道中的性能.
主要方法:
- 对声音通道历史档案观测的分析.
- 专注于500米深度以上的声音通道,在声波层以下,切断频率<200Hz.
- 观察到的声音通道发生和水质特性与数值模型输出的比较.
主要成果:
- 声音通道经常发生在罗克尔峡谷,雷克贾内斯山脊,拉布拉多流和湾流附近.
- 由于较浅的声层,在春季和夏季观察到更高的声音通道发生.
- 声道轴显示较低的盐度,表明冷,低盐度的表面水的沉积.
结论:
- 数字海洋模型分辨率 (垂直和水平) 显著影响模拟声道发生率和水质特性的准确性.
- 地下寒冷,低盐度的水受到诸如同位点潜水和冬季对流等过程的影响.
- 需要进一步考虑与水质分布和物理海洋学过程有关的模型缺陷.
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