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电离层作为近地空间环境的重要组成部分,对电波通信、卫星导航定位等都有重要影响。监测电离层形态结构有助于对电离层时空演化特征的理解及其建模和预测。随着全球导航卫星系统(global navigation satellite system,GNSS)的快速发展,GNSS电离层监测已成为重要的研究和应用方向。系统介绍了GNSS多维电离层监测及其应用的研究现状和进展,主要包括空基/地基GNSS联合反演电离层特征参数、层析技术反演电离层三维结构、电离层延迟建模、电离层异常扰动监测及机理认知等内容。 相似文献
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电离层是地球空间的重要组成部分,电离层延迟是全球导航卫星系统(global navigation satellite system,GNSS)数据处理的重要误差源,电离层的影响主要表现为地面站接收到的卫星载波和伪距信号的附加时延效应,最大可达几十米,精确的电离层模型可以有效提高GNSS单频数据处理的精度。利用GNSS观测值研究电离层,一般采用无几何距离组合的码和相位观测值,使用相位平滑伪距方法得到平滑电离层观测值,但是该方法容易受到伪距多路径和观测噪声的影响,导致电离层估计不准确。因此,先基于非组合精密单点定位(precise point positioning,PPP)提取电离层,利用国际GNSS服务的轨道、钟差等产品,有效减少待估参数个数,提高电离层延迟的估计精度;再使用纬度差和太阳时角差的多项式拟合进行区域电离层建模。利用某省连续运行参考站系统数据提取了天顶方向总电子含量信息进行建模,与PPP解算结果进行比较,在测站天顶方向上的模型值和解算值差异较小(除个别卫星外),可达到2 TECU左右。 相似文献
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电离层延迟是GNSS导航定位中重要的误差源,对电离层进行监测和建模具有重要的意义。GNSS具有覆盖范围广、观测时间长、反演精度高等特点,为电离层监测和建模提供了一种有效的手段。差分码偏差(differential code bias,DCB)包含在电离层观测值中,与电离层总电子含量(total electron content,TEC)参数相互耦合,在电离层建模时需要被精确分离和确定。 相似文献
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电离层延迟是影响导航定位精度的最主要因素。北斗卫星导航系统采用Klobuchar模型修正单频接收机用户的电离层延迟误差,对于双频接收机,可以利用不同频率信号的伪距观测数据解算得到电离层延迟值。为比较两种方法在天津地区的电离层延迟修正效果,利用NovAtel GPStation6接收机(GNSS电离层闪烁和TEC监测接收机)采集到的卫星实测数据进行计算。以国际全球导航卫星系统服务组织(IGS)发布的全球电离层格网数据为参考,对两种方法的修正效果进行比较分析。结果表明,在天津地区,利用双频观测值解算电离层延迟比Klobuchar模型计算结果更加精确,且平均每天的修正值达到IGS发布数据的82.11％,比Klobuchar模型计算值高948％ 相似文献
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电离层误差严重影响着GNSS的定位精度,GPS、BDS、Galileo、GLONASS有不同的电离层误差校正方法.全文概述了电离层误差校正方法,综述了单频电离层误差校正、双频电离层误差校正及多频电离层误差校正等技术的原理与发展现状.在单频电离层误差校正技术中总结了增强系统中的电离层误差校正技术、北斗全球电离层延迟修正模型(BeiDou global ionospheric delay correction model,BDGIM)、Klobuchar模型、单频电离层误差校正技术的优化—附加国际参考电离层(international reference ionosphere,IRI)约束模型和NeQuick-G模型;在双频电离层误差校正技术中重点总结了双频消电离层误差、无电离层组合模型及PPP-RTK技术中电离层误差校正方法;在多频电离层误差校正技术中介绍了高阶项改正和地磁场建模对电离层误差校正技术的优化与改进.最后,对电离层误差校正技术及其改进方法进行了分析,总结了其发展趋势与方向. 相似文献
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根据中国地形分布难以建立格网模型的特点,为了解决我国区域电离层精确改正的问题,提出了广域电离层改正三角分区的方法。选择中国地震电离层监测实验网中纬度地区的5个监测站,建立覆盖我国中纬度整个网络服务区域的三角分区电离层模型,并利用8个基准站的数据对该方法的修正精度进行评估,结果表明,对于三角分区内部区域,该方法可以修正到90%左右;对于三角分区外部几百公里以内的区域该方法也能达到80%以上的修正精度,同时利用原始GNSS数据对美国、加拿大等4个IGS跟踪站进行补充实验也验证了该方法的可行性,在保证模型精度的同时较格网法更加简单、有效,对广域电离层延迟误差的修正具有重要的参考价值。 相似文献
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通过实测GNSS(global navigation satellite system)数据的动态差分后处理（post processed kinematic,PPK）,对无验潮测深中的GNSS定位影响因素进行了分析,结果表明：（1）海面环境的多路径效应大于陆地环境,基准站多路径效应集中在0.15～0.3 m,而流动站则主要集中在0.3～0.5 m,对于多路径效应这类难以模型化的误差,可以通过观测环境的优化选择、GNSS接收机的软硬件升级和改良来削弱其影响。（2）粤港澳大湾区电离层较为活跃,尤其是在下午时段,当基准站距离船载移动站较远时,电离层影响的空间相关性明显降低,GNSSPPK定位方式无法很好地消减电离层延迟,测深结果受到影响较大,可以采取加设距离较近的基准站、合理安排作业时间等措施来缓解电离层延迟对GNSS定位的影响。 相似文献
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胡广保 《测绘与空间地理信息》2020,(3):153-156
针对实时GNSS单频定位中电离层延迟改正问题,本文采用可用于实时GNSS单频定位的几种电离层模型对电离层延迟进行改正并分析其对GNSS单频单点定位性能的影响。其中,对单频SPP的电离层延迟采用模型直接进行改正,采用Klobuchar模型、CODE的预报产品c1pg、原国家测绘地理信息局的实时球谐电离层产品cosong和CODE事后产品codg计算的电离层精度依次提高;采用不同电离层模型作为电离层估计的先验约束进行单频PPP定位。结果表明:采用精度较好的电离层产品作为先验约束可加快单频PPP收敛。 相似文献
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Ionospheric correction using NTCM driven by GPS Klobuchar coefficients for GNSS applications 总被引：1，自引：1，他引：0
Global Navigation Satellite Systems (GNSS) require mitigation of ionospheric propagation errors because the ionospheric range errors might be larger than tens of meters at the zenith direction. Taking advantage of the frequency-dispersive property of ionospheric refractivity, the ionospheric range errors can be mitigated in dual-frequency applications to a great extent by a linear combination of carrier phases or pseudoranges. However, single-frequency GNSS operations require additional ionospheric information to apply signal delay or range error corrections. To aid single-frequency operations, the global positioning system (GPS) broadcasts 8 coefficients as part of the navigation message to drive the ionospheric correction algorithm (ICA) also known as Klobuchar model. We presented here an ionospheric correction algorithm called Neustrelitz TEC model (NTCM) which can be used as complementary to the GPS ICA. Our investigation shows that the NTCM can be driven by Klobuchar model parameters to achieve a significantly better performance than obtained by the mother ICA algorithm. Our research, using post-processed reference total electron content (TEC) data from more than one solar cycle, shows that on average the RMS modeled TEC errors are up to 40% less for the proposed NTCM model compared to the Klobuchar model during high solar activity period, and about 10% less during low solar activity period. Such an approach does not require major technology changes for GPS users rather requires only introducing the NTCM approach a complement to the existing ICA algorithm while maintaining the simplicity of ionospheric range error mitigation with an improved model performance. 相似文献
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2020年6月23日,我国北斗三号全球导航卫星系统正式完成星座全球组网。北斗三号全球导航卫星系统采用新一代全球广播电离层延迟修正模型(BDGIM),为用户提供电离层延迟改正服务。本文利用高精度全球电离层格网(GIM)以及实测BDS/GPS数据提供的电离层TEC作为参考,从延迟改正精度及北斗单频伪距单点定位应用、模型系数性能等方面,对北斗三号系统组网前后(2020年5月1日至2020年7月20日)BDGIM模型的改正精度等应用性能进行了分析与研究,并将其与美国GPS播发的Klobuchar模型和北斗二号卫星导航系统播发的BDS Klobuchar模型进行对比。研究表明,BDGIM模型在对北斗三号系统组网完成前后电离层延迟修正精度没有发生显著变化。上述时段内,以国际GNSS服务(IGS)发布的最终GIM产品为参考,BDGIM模型在中国区域、亚太地区和全球范围内的电离层修正百分比分别达到84.45%、74.74%和64.57%;以选取的全球83个GNSS检测站BDS、GPS双频数据实测电离层TEC为参考,BDGIM在中国区域、亚太地区和全球范围内的电离层修正百分比分别为73.12%、70.18%及68.06%;当BDGIM模型应用于北斗单频伪距单点定位时,在中国区域、亚太地区和全球范围内分别实现了2.22、2.66和2.96 m的三维定位精度。 相似文献
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Processing of data from global navigation satellite systems (GNSS), such as GPS, GLONASS and Galileo, can be considerably impeded by disturbances in the ionosphere. Cycle-slip detection and correction thus becomes a crucial component of robust software. Still, dealing with ionospheric cycle slips is not trivial due to scintillation effects in both the phase and the amplitude of the signals. In this contribution, a geometry-based approach with rigorous handling of the ionosphere is presented. A detailed analysis of the cycle-slip correction process is also tackled by examining its dependence on phase and code noise, non-dispersive effects and, of course, the ionosphere. The importance of stochastic modeling in validating the integer cycle-slip candidates is emphasized and illustrated through simulations. By examining the relationship between ionospheric bias and ionospheric constraint, it is shown that there is a limit in the magnitude of ionospheric delay variation that can be handled by the cycle-slip correction process. Those concepts are applied to GNSS data collected by stations in northern Canada, and show that enhanced cycle-slip detection can lead to decimeter-level improvements in the accuracy of kinematic PPP solutions with a 30-s sampling interval. Cycle-slip correction associated with ionospheric delay variations exceeding 50 cm is also demonstrated, although there are risks with such a procedure and these are pointed out. 相似文献
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Application of SWACI products as ionospheric correction for single-point positioning: a comparative study 总被引：1，自引：0，他引：1
In Global Navigation Satellite Systems (GNSS) using L-band frequencies, the ionosphere causes signal delays that correspond with link related range errors of up to 100 m. In a first order approximation the range error is proportional to the total electron content (TEC) of the ionosphere. Whereas this first order range error can be corrected in dual-frequency measurements by a linear combination of carrier phase- or code-ranges of both frequencies, single-frequency users need additional information to mitigate the ionospheric error. This information can be provided by TEC maps deduced from corresponding GNSS measurements or by ionospheric models. In this paper we discuss and compare different ionospheric correction methods for single-frequency users. The focus is on the comparison of the positioning quality using dual-frequency measurements, the Klobuchar model, the NeQuick model, the IGS TEC maps, the Neustrelitz TEC Model (NTCM-GL) and the reconstructed NTCM-GL TEC maps both provided via the ionosphere data service SWACI (http://swaciweb.dlr.de) in near real-time. For that purpose, data from different locations covering several days in 2011 and 2012 are investigated, including periods of quiet and disturbed ionospheric conditions. In applying the NTCM-GL based corrections instead of the Klobuchar model, positioning accuracy improvements up to several meters have been found for the European region in dependence on the ionospheric conditions. Further in mid- and low-latitudes the NTCM-GL model provides results comparable to NeQuick during the considered time periods. Moreover, in regions with a dense GNSS ground station network the reconstructed NTCM-GL TEC maps are partly at the same level as the final IGS TEC maps. 相似文献