Spatiotemporal Analysis of Sonar Detection Range in Luzon Strait

Gengming Zhang, Lihua Zhang, Yitao Wang, Yaowei Ma, Xingyu Zhou, Yue Yu
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Abstract

Sonar serves as a critical submarine detection apparatus for naval vessels, with its detection range forming the foundation of its overall performance in underwater surveillance. The Luzon Strait, in the eastern part of the South China Sea, presents a complex hydrographic setting that profoundly influences sonar performance, necessitating mastery of the detection range variation for enhanced anti-submarine operational efficiency. This study employs the Bellhop acoustic propagation model to estimate the transmission loss. Subsequently, a detection probability integration approach is applied to determine the sonar detection range in the Luzon Strait from 2019 to 2023, which is then subjected to statistical analysis. The findings indicate the following. (1) During the summer and autumn, the shallow mixed layer fails to generate a surface duct, resulting in shorter detection ranges that are primarily dependent on the water depth. In the Shallow Water Zone (<150 m), frequent interactions between sound waves and the sea boundaries lead to considerable acoustic energy attenuation, maintaining a short detection range. In the Intermediate Depth Zone (150–2500 m), sound rays retain adequate energy post-seabed reflection, extending the sonar detection to 5–8 km. Beyond 2500 m, the diminishing reflective energy restricts the range to 2–5 km. (2) Conversely, in the winter and spring, the formation of a surface duct becomes the predominant determinant of the detection range, capable of exceeding 10 km, overshadowing the influence of the water depth.
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吕宋海峡声纳探测范围的时空分析
声纳是海军舰艇探测潜艇的关键设备,其探测范围是水下监视整体性能的基础。位于中国南海东部的吕宋海峡水文环境复杂,对声纳性能影响深远,因此必须掌握探测距离的变化,以提高反潜作战效率。本研究采用 Bellhop 声学传播模型来估算传输损耗。随后,采用探测概率整合方法确定 2019 年至 2023 年吕宋海峡的声纳探测范围,并对其进行统计分析。研究结果表明(1) 在夏秋季节,浅层混合层无法产生表面导管,导致探测距离较短,而探测距离 主要取决于水深。在浅水区(小于 150 米),声波与海洋边界之间频繁的相互作用导致相当大的声能衰减,从而保持较短的探测距离。在中深水区(150-2500 米),声波在海底反射后仍能保持足够的能量,从而将声纳探测范围扩大到 5-8 千米。超过 2500 米后,反射能量的减少将探测距离限制在 2-5 千米。(2) 相反,在冬季和春季,海面导管的形成成为探测距离的主要决定因素,探测距离可超过 10 千米,超过了水深的影响。
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