使用GNSS信号和陆地蜂信号的多时代差异化伪范围联合定位机会信号
Pei Zhang1, Tian Jin1, James Chakwizira2
1School of Electronic and Information Engineering, Beihang University, Beijing 100191, China.
Sensors (Basel, Switzerland)
|September 27, 2025
概括
本研究介绍了一种新的蜂和全球导航卫星系统 (GNSS) 融合定位模型,用于低信号环境. 该方法提高了准确性,避免了初始位置的需求,改善了GNSS无法使用的导航.
科学领域:
- 导航系统 导航系统
- 信号处理 信号处理
- 地理学工程 工程地质学
背景情况:
- 全球导航卫星系统 (GNSS) 对于定位至关重要,但在低可观测性环境中失败.
- 蜂机遇信号 (SOP) 提供了一个替代方案,但由于初始化困难和时空不确定性,在GNSS的融合定位方面面临挑战.
- 当前的方法在GNSS和蜂信号有限时,难以精确的位置初始化和管理不确定性.
研究的目的:
- 提出一种新的蜂SOP和GNSS信号融合定位模型,以克服在低可观测性环境中的局限性.
- 解决融合定位中精确位置初始化和时空不确定性的挑战.
- 在GNSS可用性受到损害时,提高定位系统的稳定性和准确性.
主要方法:
- 开发了一种使用伪范围单差在多时代 (PSDM) 的蜂SOP和GNSS信号融合定位模型.
- 差异化伪色被用来解决融合定位的时空不确定性.
- 一种伪线性化的封闭形式方法被衍生和重建,导致一个受约束的多步加权最小方程 (CMWLS) 方法,以减轻噪声和改善收.
主要成果:
- 拟议的PSDM模型有效地解决了使用差异化伪范围的时空不确定性.
- 重建的伪线性化和CMWLS方法克服了精确位置初始化方面的挑战.
- 模拟和实地测试在低可观测性环境中显示出良好的定位性能,优于现有方法.
结论:
- 开发的蜂SOP和GNSS信号融合定位方法为在GNSS可用性有限的环境中导航提供了可行的解决方案.
- 这种方法成功地减轻了初始化困难和时空不确定性,提供了更好的定位精度.
- 该研究提出了城市定位的新策略,消除了对先前接收器位置信息的需求.
相关概念视频
Errors in Global Positioning System
338
Global Positioning System (GPS) technology has revolutionized navigation and positioning, but its accuracy is often compromised by various errors. These errors, stemming from environmental, satellite, and receiver-related factors, require careful mitigation to ensure reliable performance across applications.Atmospheric ErrorsGPS signals travel through the Earth’s ionosphere and troposphere, introducing delays which affect accuracy. The ionosphere is strongly influenced by charged particles,...
338
Types of Global Positioning System Surveys
347
GPS surveying methods vary in application, accuracy, and data collection techniques, catering to diverse surveying and mapping needs. Static GPS, kinematic GPS, and real-time kinematic (RTK) surveying are widely used. Each technique offers distinct advantages.Static GPS involves placing one receiver at a known reference point and another at the target point. It collects exact positional data by observing multiple satellite ranges over an extended period, achieving centimeter-level accuracy for...
347
Field Application of Global Positioning System
322
The Global Positioning System (GPS) has become an indispensable tool in fieldwork, offering unparalleled precision and efficiency for surveying, navigation, and infrastructure development. By harnessing signals from a constellation of satellites, GPS receivers determine the location of objects with remarkable speed and accuracy, often completing calculations within a second.Advantages of Modern GPS TechnologyContemporary GPS receivers are designed to meet the practical demands of field...
322
Design Example: Identifying the Locations of Monuments in the Field Using Global Positioning System Device
379
Surveyors use Global Positioning System (GPS) technology to measure the precise location and elevation of points on Earth. In a recent survey, GPS receivers were used to determine the coordinates and elevations of two park monuments. The process involved careful mission planning, data collection, and correction to ensure accuracy. The survey began with mission planning to identify optimal satellite visibility and minimize Position Dilution of Precision (PDOP). A geodetic control point...
379
Introduction to Global Positioning System
465
The Global Positioning System (GPS) revolutionized positioning on Earth, providing precise location data through satellite ranging. The GPS system was developed in 1978 by the U.S. Department of Defense for military use, and it became available for civilian applications in 1983, transforming fields including navigation, fleet management, and time synchronization for telecommunications systems.GPS consists of satellites in medium Earth orbit, about 20,200 kilometers above the surface,...
465
Geoid and Ellipsoid
599
The Earth's shape is best described as an ellipsoid, a slightly flattened sphere created by rotating an ellipse around its minor axis. This flattening results in the polar axis being about 21 kilometers shorter than the equatorial axis. In contrast, the geoid represents the Earth's gravitational shape and aligns with the mean sea level (MSL). The geoid is an irregular equipotential surface where gravity is perpendicular at every point. Variations in Earth's mass distribution cause geoid...
599


