Assessment of GNSS PPP-Based Zenith Tropospheric Delay

IF 0.7 Q4 ASTRONOMY & ASTROPHYSICS Artificial Satellites-Journal of Planetary Geodesy Pub Date : 2020-12-01 DOI:10.2478/arsa-2020-0012
M. Abdelazeem, A. El-Rabbany
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引用次数: 1

Abstract

Abstract This study assesses the precision of zenith tropospheric delay (ZTD) obtained through triple-constellation global navigation satellite system (GNSS) precise point positioning (PPP). Various ZTD estimates are obtained as by-products from GPS-only, GPS/Galileo, GPS/BeiDou, and triple-constellation GPS/Galileo/BeiDou PPP solutions. Triple-constellation GNSS observations from a number of globally distributed reference stations are processed over a period of seven days in order to investigate the daily performance of the ZTD estimates. The estimated ZTDs are then validated by comparing them with the International GNSS Service (IGS) tropospheric products and the University of New Brunswick (UNB3m) model counterparts. It is shown that the ZTD estimates agree with the IGS counterparts with a maximum standard deviation (STD) of 2.4 cm. It is also shown that the precision of estimated ZTD from the GPS/Galileo and GPS/Galileo/BeiDou PPP solutions is improved by about 4.5 and 14%, respectively, with respect to the GPS-only PPP solution. Moreover, it is found that the estimated ZTD agrees with the UNB3m model with a maximum STD of 3.1 cm. Furthermore, the GPS/Galileo and GPS/Galileo/BeiDou PPP enhance the precision of the ZTD estimates by about 6.5 and 10%, respectively, in comparison with the GPS-only PPP solution.
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基于ppp的GNSS天顶对流层延迟评估
摘要本研究评估了通过三星座全球导航卫星系统(GNSS)精确点定位(PPP)获得的天顶对流层延迟(ZTD)的精度。各种ZTD估计是从仅GPS、GPS/Gileo、GPS/北斗和三星座GPS/Gileo/北斗PPP解决方案中获得的副产品。在七天的时间里,对来自全球分布的一些参考站的全球导航卫星系统三星座观测进行了处理,以调查ZTD估计的日常表现。然后,通过将估计的ZTD与国际全球导航卫星系统服务(IGS)对流层产品和新不伦瑞克大学(UNB3m)模型的对应产品进行比较,对其进行验证。结果表明,ZTD估计值与IGS对应值一致,最大标准偏差(STD)为2.4cm。还表明,与仅GPS的PPP解决方案相比,GPS/Gileo和GPS/Gileo/北斗PPP解决方案估计的ZTD精度分别提高了约4.5%和14%。此外,我们发现估计的ZTD与UNB3m模型一致,最大STD为3.1cm。此外,与仅使用GPS的PPP解决方案相比,GPS/Gileo和GPS/Gileo/北斗PPP分别将ZTD估计的精度提高了约6.5%和10%。
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