Single-Frequency Ionospheric-Delay Correction from BeiDou & GPS Systems for Northern Hemisphere

IF 0.7 Q4 ASTRONOMY & ASTROPHYSICS
A. Farah
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引用次数: 2

Abstract

Abstract The range delay caused by the ionosphere layer is the major current source of error for GNSS users with single-frequency receivers. GNSS advice users to correct this type of error using ionospheric models whose coefficients are sent in their navigation messages. GPS-users use the Klobuchar model to correct this type of error. GPS navigation message contains the model’s eight coefficients which vary on the basis of seasonal ionospheric variations and average solar flux. The correction accuracy of Klobuchar model is about 50% (rms) of the ionospheric range delay. Beidou system calculates and broadcast 8 parameters of Klobuchar model based on continuous monitoring stations. BeiDou system updates the ionospheric coefficients every two hours. GPS-Klobuchar model uses completely different coefficients than BeiDou-Klobuchar model. This research demonstrates a comparison study between the Klobuchar model using the GPS broadcast coefficients and the same model using BeiDou-coefficients. The correction accuracy offered by the two models has been judged using the most accurate International GNSS Service-Global Ionospheric Maps (IGS-GIMs) for three different-latitude stations along northern hemisphere, one station in low-latitude region, the second station is in mid-latitude region and the third station is in high-latiude region to reflect models’ behaviour in different geographic regions. The study was applied over three different months of the year 2017 that each of them reflects a different activity state for the ionosphere layer. The study proves that BeiDou model is able to show the ionosphere’s day-to-day fluctuations while GPS model can’t. It can be concluded that GPS model offers better behaviour than BeiDou model in correcting range delay in low-latitude and high-latitude geographic regions under any activity state for the ionosphere. BeiDou model offers better correction accuracy than GPS model in mid-latitude under any activity state for the ionosphere.
北斗和全球定位系统对北半球电离层单频延迟的校正
摘要电离层层引起的距离延迟是目前使用单频接收机的GNSS用户的主要误差源。全球导航卫星系统建议用户使用电离层模型来纠正这类错误,电离层模型的系数在其导航消息中发送。GPS用户使用Klobuchar模型来纠正这种类型的错误。GPS导航信息包含该模型的八个系数,这些系数根据电离层的季节变化和平均太阳通量而变化。Klobuchar模型的校正精度约为电离层距离延迟的50%(rms)。北斗系统基于连续监测站计算并广播Klobuchar模型的8个参数。北斗系统每两小时更新一次电离层系数。GPS Klobuchar模型使用的系数与北斗Klobucher模型完全不同。本研究展示了使用GPS广播系数的Klobuchar模型与使用北斗系数的相同模型之间的比较研究。这两个模型提供的校正精度是使用最准确的国际GNSS服务全球电离层图(IGS-GIM)对北半球三个不同纬度的台站、一个低纬度地区的台站和一个低纬地区的台站进行判断的,第二个站位于中纬度地区,第三个站位于高纬度地区,以反映模型在不同地理区域的行为。这项研究应用于2017年的三个不同月份,每个月都反映了电离层的不同活动状态。研究证明,北斗模型能够显示电离层的日常波动,而GPS模型则不能。结果表明,在电离层的任何活动状态下,GPS模型在低纬度和高纬度地理区域的距离延迟校正方面都比北斗模型具有更好的性能。在任何电离层活动状态下,北斗模型在中纬度都比GPS模型具有更好的校正精度。
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CiteScore
1.00
自引率
11.10%
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