Accuracy Assessment Study of UNB3m Neutral Atmosphere Model for Global Tropospheric Delay Mitigation

IF 0.7 Q4 ASTRONOMY & ASTROPHYSICS
A. Farah
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引用次数: 3

Abstract

Abstract Tropospheric delay is the second major source of error after the ionospheric delay for satellite navigation systems. The transmitted signal could face a delay caused by the troposphere of over 2m at zenith and 20m at lower satellite elevation angles of 10 degrees and below. Positioning errors of 10m or greater can result from the inaccurate mitigation of the tropospheric delay. Many techniques are available for tropospheric delay mitigation consisting of surface meteorological models and global empirical models. Surface meteorological models need surface meteorological data to give high accuracy mitigation while the global empirical models need not. Several hybrid neutral atmosphere delay models have been developed by (University of New Brunswick, Canada) UNB researchers over the past decade or so. The most widely applicable current version is UNB3m, which uses the Saastamoinen zenith delays, Niell mapping functions, and a look-up table with annual mean and amplitude for temperature, pressure, and water vapour pressure varying with respect to latitude and height. This paper presents an assessment study of the behaviour of the UNB3m model compared with highly accurate IGS-tropospheric estimation for three different (latitude/height) IGS stations. The study was performed over four nonconsecutive weeks on different seasons over one year (October 2014 to July 2015). It can be concluded that using UNB3m model gives tropospheric delay correction accuracy of 0.050m in average for low latitude regions in all seasons. The model's accuracy is about 0.075m for medium latitude regions, while its highest accuracy is about 0.014m for high latitude regions.
全球对流层延迟减缓UNB3m中性大气模式的精度评估研究
对流层时延是卫星导航系统中仅次于电离层时延的第二大误差源。由于对流层在天顶和卫星仰角在10度及以下的较低位置会造成2米以上和20米以上的延迟,因此传输信号可能面临延迟。对流层延迟的不准确缓解可能导致10米或更大的定位误差。可用于减缓对流层延迟的技术有许多,包括地面气象模式和全球经验模式。地面气象模式需要地面气象资料才能提供高精度的减缓,而全球经验模式则不需要。在过去十年左右的时间里,加拿大新不伦瑞克大学UNB的研究人员开发了几种混合中性大气延迟模型。目前应用最广泛的版本是UNB3m,它使用了Saastamoinen天顶延迟,Niell绘图功能,以及温度、压力和水蒸气压力随纬度和高度变化的年平均值和振幅的查找表。本文对UNB3m模式的行为进行了评估研究,并将其与三个不同(纬度/高度)的IGS站的高精度对流层估计进行了比较。该研究在一年内(2014年10月至2015年7月)的不同季节进行了四个非连续周的研究。结果表明,采用UNB3m模式对低纬度地区各季节的对流层延迟校正精度平均为0.050m。模型在中纬度地区的精度约为0.075m,在高纬度地区的最高精度约为0.014m。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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CiteScore
1.00
自引率
11.10%
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0
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