一种参考相位速度选择的方法,用于在浅水中使用水平线阵列进行轴承估计
Dai Liu1, Feilong Zhu1, Yanjun Zhang1
1State Key Laboratory of Acoustics, Institute of Acoustics, Chinese Academy of Sciences, Beijing 100190, Chinaliudai@mail.ioa.ac.cn, zhufl@mail.ioa.ac.cn, zhangyanjun@mail.ioa.ac.cn, pzh@mail.ioa.ac.cn.
JASA express letters
|March 12, 2025
概括
选择正确的参考相速对于使用水平线阵列进行准确的水下源轴承估计至关重要. 这项研究引入了一种新的方法,以提高浅水的定向精度.
科学领域:
- 声学 声学 在声学方面
- 海洋学 海洋学 海洋学
- 信号处理 信号处理
背景情况:
- 准确的到达方向 (DOA) 估计对于水下声源定位至关重要.
- 在浅水中,参考相位速度的选择显著影响了DOA估计准确度,使用梁形水平线阵列.
- 不匹配的参考相速导致估计的源轴承偏差.
研究的目的:
- 分析参考相速与影响DOA估计的因素之间的关系.
- 开发一种改进的方法来选择浅水环境中的参考相速.
- 为了提高源轴承估计的准确性,使用水下水平线阵列.
主要方法:
- 分析参考相速,正常模式振幅分布,源轴承和阵列孔径之间的内在关系.
- 开发一个多参数加权的参考阶段速度选择方法.
- 通过数值模拟和实验数据进行验证.
主要成果:
- 在参考相速和正常模式特征之间发现了直接的相关性.
- 与传统方法相比,拟议的多参数加权方法在源轴承估计中显示出更高的准确性.
- 由于速度不匹配而导致估计轴承的偏差被量化.
结论:
- 拟议的方法有效地提高了在浅水环境中源轴承估计的准确性.
- 准确的参考相速率选择对于使用水平线阵列可靠的DOA估计至关重要.
- 这些发现得到了数字模拟和实验结果的验证.
相关概念视频
Influence of Earth's Curvature and Atmospheric Refraction on Leveling
30
During leveling, the Earth's curvature and atmospheric refraction introduce deviations in the line of sight from a true horizontal reference. When the line of sight is leveled, it remains perpendicular to the plumb line only at a single point. Beyond this, it deviates due to the Earth’s curvature, represented by the correction C. For a sight distance D, the deviation can be derived using the relationship:This relationship shows that the deviation increases quadratically with distance.
30
Design Example: Measuring Distance Between Two Points with Obstructions
17
When measuring distances in areas with physical obstructions, such as a lake in a field, surveyors must employ techniques to calculate accurate lengths without direct line measurements. One effective method is the offset technique, which allows for precise distance estimation over inaccessible stretches.In this scenario, a surveyor must measure a side of an area that crosses a lake. Since the measuring tape cannot span the lake, the surveyor begins by establishing a baseline that aligns with...
17
Azimuths and Bearings
45
Azimuths and bearings are essential concepts in surveying, providing methods to express the direction of a line relative to a meridian. Azimuths refer to the clockwise angle measured from the north end of a reference meridian to the given line, ranging from zero to 360 degrees. This method gives a comprehensive directional reference within a full 360-degree circle, making it a straightforward way to communicate direction in various fields, including navigation, cartography, and...
45
Relative Motion Analysis using Rotating Axes-Problem Solving
369
Consider a crane whose telescopic boom rotates with an angular velocity of 0.04 rad/s and angular acceleration of 0.02 rad/s2. Along with the rotation, the boom also extends linearly with a uniform speed of 5 m/s. The extension of the boom is measured at point D, which is measured with respect to the fixed point C on the other end of the boom. For the given instant, the distance between points C and D is 60 meters.
Here, in order to determine the magnitude of velocity and acceleration for point...
Here, in order to determine the magnitude of velocity and acceleration for point...
369
Differential Leveling
85
Differential leveling is a precise method in surveying used to determine the elevation difference between two points. Its primary goal is to establish accurate vertical measurements to create level surfaces or grade lines critical for designing and constructing infrastructures such as roads, bridges, and buildings.The procedure for differential leveling begins with setting up and leveling the instrument at a point where the benchmark can be seen. The level rod is held on the benchmark (BM), and...
85
Relative Velocity in Two Dimensions
6.6K
Relative velocity is the velocity of an object as observed from a particular reference frame, or the velocity of one reference frame with respect to another reference frame. The concept of relative velocity can be used to describe motion in two dimensions. Consider a particle P and two reference frames S and S′. The position of the origin of S′ as measured in S is , the position of P as measured in S′ is , and the position of P as measured in S is , which can be evaluated by...
6.6K


