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Ionospheric tomography by gradient enhanced kriging with STEC measurements and ionosonde characteristics

机译:通过STEC测量和离子探空仪特性的梯度增强克里金法进行电离层层析成像

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摘要

The estimation of the ionospheric electron density by kriging is based on the optimization of a parametric measurement covariance model. First, the extension of kriging with slant total electron content (STEC) measurements based on a spatial covariance to kriging with a spatial-temporal covariance model, assimilating STEC data of a sliding window, is presented. Secondly, a novel tomography approach by gradient enhanced kriging (GEK) is developed. Beyond the ingestion of STEC measurements, GEK assimilates ionosonde characteristics providing peak electron density measurements as well as\udgradient information. Both approaches deploy the 3D electron density model NeQuick as a priori information and estimate the covariance parameter vector within a maximum likelihood estimation for the dedicated tomography time stamp. The methods are validated in the European region for two periods covering quiet and active ionospheric conditions. The kriging with spatial\udand spatial-temporal covariance model is analysed regarding its capability to reproduce STEC, differential STEC and foF2. Therefore the estimates are compared to the NeQuick model results, the 2D TEC maps of the International GNSS Service and the DLR’s Ionospheric Monitoring and Prediction Center, and in case of foF2 to two independent ionosonde stations. Moreover,\udsimulated STEC and ionosonde measurements are used to investigate the electron density profiles estimated by the GEK in comparison to a kriging with STEC only. The results indicate a crucial improvement in the initial guess by the developed methods and point out the potential compensation for a bias in the peak height hmF2 by means of GEK.
机译:通过克里格法估算电离层电子密度是基于参数测量协方差模型的优化。首先,提出了将基于空间协方差的倾斜总电子含量(STEC)测量的克里金法扩展到使用时空协方差模型的克里金方法,该方法吸收了滑动窗口的STEC数据。其次,开发了一种通过梯度增强克里金法(GEK)的新型层析成像方法。除了摄取STEC测量值外,GEK还可以吸收离子探空仪特性,从而提供峰值电子密度测量值和\梯度信息。两种方法都将3D电子密度模型NeQuick部署为先验信息,并在专用断层摄影时间戳的最大似然估计中估计协方差参数矢量。该方法在欧洲地区经过两次验证,涵盖了安静和活跃的电离层状况。分析了具有空间\ udand时空协方差模型的kriging能够再现STEC,差分STEC和foF2的能力。因此,将估算值与NeQuick模型结果,国际GNSS服务的2D TEC地图以及DLR的电离层监测和预测中心进行比较,在foF2情况下,将其与两个独立的电离探空仪站进行比较。此外,模拟的STEC和离子探空仪测量结果用于研究GEK估计的电子密度分布图,与仅使用STEC的克里金法相比。结果表明,通过开发的方法,可以对初始猜测进行重大改进,并指出可以通过GEK补偿峰高hmF2的偏差。

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