电离层闪烁下伽利略跟踪鲁棒性的积分时间延长

N. Kassabian, Y. Morton
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引用次数: 8

摘要

随着越来越多的业务和应用越来越依赖全球导航卫星系统(GNSS)技术,其连续性要求自然也变得更加严格。电离层闪烁现象是威胁这些连续性要求的主要问题之一。它导致无线电频率(RF)信号的幅度、相位和频率波动,穿过空间,穿透电离层,数百公里的高度,在那里,来自太阳风的湍流电离气体或等离子体改变了电磁信号的特征。本文的目的是研究GNSS标量跟踪环路中使用的相干积分间隔的延长对保持欧洲GNSS伽利略E1开放服务(OS)信号的跟踪或同步的影响。为此,在数字域设计了一阶最优环路滤波器,最优地减小了瞬态能量和热噪声跟踪抖动。并通过根轨迹和波德样地对其稳定性和稳定度进行了理论研究。并将其性能与文献中常用的传统模拟环路滤波器进行了比较。在模拟微弱伽利略信号和受闪烁影响的模拟信号上,对采用该滤波器的载波和码跟踪环路进行了测试。首先分别考虑快速和缓慢的幅度和相位闪烁,以了解每个变量(幅度/相位)的机制,然后将这两种波动合并到模拟的伽利略信号中。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Extending integration time for Galileo tracking robustness under ionosphere scintillation
As a wide array of services and applications are becoming more reliant on Global Navigation Satellite System (GNSS) technology, its continuity requirements are naturally becoming more stringent. The ionosphere scintillation phenomenon is one of the major concerns that threaten these continuity requirements. It results in amplitude, phase and frequency fluctuations of Radio Frequency (RF) signals traveling through space and piercing the ionosphere, hundreds of Km of altitude, where turbulent ionized gases or plasma that stem from solar winds modify the characteristics of electromagnetic signals. The objective of this paper is to study the impact of extending the coherent integration interval used in GNSS scalar tracking loops, in terms of maintaining tracking or synchronization of the European GNSS Galileo E1 Open Service (OS) signals. For that end, a first order optimum loop filter is designed in the digital domain, optimal in minimizing both transient energy and thermal noise tracking jitter. Moreover, a theoretical study of its stability and degree of stability is carried out through root locus and Bode plots. Its performance is also compared to that of traditional analog loop filters often used in literature. Carrier and code tracking loops using this optimum digital loop filter are tested on simulated weak Galileo signals as well as simulated scintillation affected signals. Fast and slow amplitude, phase scintillation are first considered separately to understand the mechanisms of each variable (amplitude/phase), and then both fluctuations are incorporated onto the simulated Galileo signal.
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