Validation of regional and global ionosphere maps from GNSS measurements versus IRI2016 during different magnetic activity

IF 1.2 Q4 REMOTE SENSING
A. Sedeek
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引用次数: 2

Abstract

Abstract This manuscript explores the divergence of the Vertical Total Electron Content (VTEC) estimated from Global Navigation Satellite System (GNSS) measurements using global, regional, and International Reference Ionosphere (IRI) models over low to high latitude regions during various magnetic activity. The VTEC is estimated using a territorial network consisting of 7 GNSS stations in Egypt and 10 GNSS stations from the International GNSS Service (IGS) Global network. The impact of magnetic activity on VTEC is investigated. Due to the deficiency of IGS receivers in north Africa and the shortage of GNSS measurements, an extra high interpolation is done to cover the deficit of data over North Africa. A MATLAB code was created to produce VTEC maps for Egypt utilizing a territorial network contrasted with global maps of VTEC, which are delivered by the Center for Orbit Determination in Europe (CODE). Thus we can have genuine VTEC maps estimated from actual GNSS measurements over any region of North Africa. A Spherical Harmonics Expansion (SHE) equation was modelled using MATLAB and called Local VTEC Model (LVTECM) to estimate VTEC values using observations of dual-frequency GNSS receivers. The VTEC calculated from GNSS measurement using LVTECM is compared with CODE VTEC results and IRI-2016 VTEC model results. The analysis of outcomes demonstrates a good convergence between VTEC from CODE and estimated from LVTECM. A strong correlation between LVTECM and CODE reaches about 96 % and 92 % in high and low magnetic activity, respectively. The most extreme contrasts are found to be 2.5 TECu and 1.3 TECu at high and low magnetic activity, respectively. The maximum discrepancies between LVTECM and IRI-2016 are 9.7 TECu and 2.3 TECu at a high and low magnetic activity. Variation in VTEC due to magnetic activity ranges from 1–5 TECu in moderate magnetic activity. The estimated VTEC from the regional network shows a 95 % correlation between the estimated VTEC from LVTECM and CODE with a maximum difference of 5.9 TECu.
在不同的磁活动期间,GNSS测量与IRI2016的区域和全球电离层图的验证
摘要:本文探讨了利用全球、区域和国际参考电离层(IRI)模型在低至高纬度地区不同磁活动期间,全球导航卫星系统(GNSS)测量结果估计的垂直总电子含量(VTEC)的差异。VTEC估计使用一个由埃及的7个GNSS站和来自国际GNSS服务(IGS)全球网络的10个GNSS站组成的领土网络。研究了磁活动对VTEC的影响。由于北非缺乏IGS接收机和缺乏GNSS测量值,为了弥补北非的数据不足,进行了超高插值。创建了一个MATLAB代码,利用由欧洲轨道确定中心(code)提供的区域网络与VTEC全球地图进行对比,为埃及生成VTEC地图。因此,我们可以根据实际GNSS测量在北非任何地区估算出真正的VTEC地图。利用MATLAB对球谐展开(SHE)方程进行建模,并将其称为局部VTEC模型(LVTECM),利用双频GNSS接收机的观测值估算VTEC值。利用LVTECM计算GNSS测量的VTEC与CODE VTEC结果和iris -2016 VTEC模型结果进行了比较。结果分析表明,CODE的VTEC与LVTECM估计的VTEC具有很好的收敛性。在高、低地磁活动中,LVTECM与CODE的相关性分别达到96%和92%左右。在高和低磁活动时,对比最极端的分别为2.5 TECu和1.3 TECu。在高、低地磁活动时,LVTECM与IRI-2016的最大差异分别为9.7 TECu和2.3 TECu。磁活动引起的VTEC变化范围为1-5 TECu(中等磁活动)。从区域网络估计的VTEC与从LVTECM估计的VTEC之间的相关性为95%,最大差值为5.9 TECu。
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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来源期刊
Journal of Applied Geodesy
Journal of Applied Geodesy REMOTE SENSING-
CiteScore
2.30
自引率
7.10%
发文量
30
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