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Evaluation of three ionospheric delay computation methods for ground-based GNSS receivers

机译:基于地基GNSS接收器的三个电离层延迟计算方法的评价

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摘要

GNSS observables for ionospheric estimation are commonly based on carrier-to-code leveling (CCL) and precise point positioning (PPP) methods. The CCL method is a geometry-free method which uses carrier phase to level pseudorange observation for decreasing multipath error and observation noise. However, the ionospheric observable based on the CCL has been proven to be affected by leveling errors. The leveling errors are caused by pseudorange multipath and intraday variation of receiver DCB. To obtain more accurate ionospheric observable, the PPP method takes advantage of precise satellite-to-ground range for retrieving slant total electron content and is less affected by the leveling errors. Previous studies have only proven that the ionospheric observables extracted by the two methods are affected by the leveling errors. The influence on ionospheric observable by the pseudorange inter-receiver satellite bias (IRSB) of the receiver has not been taken into consideration. Also, the magnitude of the differences between the ionospheric observables extracted by the two methods has also not been given. In this work, three methods, namely, the CCL, the conventional ionospheric-free PPP method which uses the ionospheric-free Hatch-Melbourne-Wubbena (HMW) function, and the University of Calgary (UOFC) PPP method, are selected to analyze and compare the differences of ionospheric observables and the global ionospheric maps, using a large number of measured data from international GNSS service global stations. Experimental results show that the accuracy of ionospheric observables obtained by the three methods is not only related to the leveling error, but also pseudorange IRSB. The IRSB of the receiver exerts a major effect on the ionospheric observables obtained by the CCL method and a minor effect on the ionospheric observables obtained by the HMW and UOFC methods. The accuracies in the latter case are similar and superior to those obtained by the CCL. The differences of the
机译:电离层估计的GNSS可观察者通常基于载波到码调平(CCL)和精确点定位(PPP)方法。 CCL方法是一种几何形状的方法,它使用载波阶段进行级伪距观察,以降低多径误差和观察噪声。然而,已被证明基于CCL的电离层可观察到通过调平误差影响。调平误差是由Pseudorange多径和接收器DCB的盘子内变型引起的。为了获得更精确的电离层可观察,PPP方法利用精确的卫星到地面,用于检索倾斜的全电子含量,并且受水平误差的影响较小。以前的研究仅证明了两种方法提取的电离层可观察物受水平误差的影响。通过接收器的伪距接收器卫星偏置(IRSB)对电离层的影响尚未考虑。而且,也没有给出由两种方法提取的电离层可观察结果之间的差异的大小。在这项工作中,三种方法,即CCL,使用无电离层 - 无舱口 - 墨尔本 - 武器(HMW)功能和Calgary大学(UOFC)PPP方法的传统电离层的PPP方法,分析并比较了电离层观察和全局电离层地图的差异,使用来自国际GNSS服务全球站的大量测量数据。实验结果表明,三种方法获得的电离层观察的准确性不仅与水平误差有关,还具有伪距离IRSB。接收器的IRSB对通过CCl方法获得的电离层可观察结果的主要影响和对HMW和UOFC方法获得的电离层可观察结果的微小影响。后一种情况下的准确性相似,优于CCL获得的那些。差异的差异

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