伊明格海西部的溢出水改变了深音速结构和收区传播
EeShan C Bhatt1, Arthur B Baggeroer1,2, Robert A Weller1
1Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA.
The Journal of the Acoustical Society of America
|February 11, 2024
概括
深海的声音速度是动态的,与统一的模型不同. 精确的声学建模需要在1公里以下的位置音速数据,特别是在复杂的循环区域.
科学领域:
- 海洋学 海洋学 海洋学
- 声学 声学 在声学方面
- 地质物理学 地质物理学
背景情况:
- 全球海洋学模型通常假定声速梯度是均的.
- 西欧林格海表现出复杂,动态的深音速度结构.
- 这种不均性挑战了声传播模型.
研究的目的:
- 研究动态深音速度结构对声信号的影响.
- 为了比较声信号的行为与均与非均的声速梯度.
- 突出在现场音速数据的必要性,用于准确的远程声学研究.
主要方法:
- 采用束束源抛物线方程模型.
- 在浅水源和接收器阵列之间模拟声学传播.
- 采用光束成形分析来解释声学干扰模式.
主要成果:
- 不统一的声速结构在1-1.5公里的深度和近海底的反转显著影响声信号.
- 统一的声速梯度产生了理想化的干扰模式,这些干扰模式误导了融合区属性 (位置,强度,清晰度).
- 模拟的收区特征与统一梯度假设所预测的特征有很大不同.
结论:
- 在1公里以下的现场音速测量对于准确的低频,远程声传播研究至关重要.
- 复杂的热环流区域需要详细的,局部化的声速数据.
- 目前的全球建模方法可能需要改进,以考虑到海洋声速的动态变化.
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