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Imaging the Ionospheric Electron Density Using a Combined Tomographic Algorithm

机译:使用组合断层算法成像电离层电子密度

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A new algorithm, which is the combination of the generalized singular value decomposition (GSVD) and the improved algebraic reconstruction technique (IART), is proposed to image ionospheric electron density (IED) distribution in this paper. In this new method, the GSVD is first used to resolve the ill-posed problem in computerized ionospheric tomography (CIT) system. Its estimate inverted from total electron content (TEC) measurements is then provided as the initial approximation required by the IART. The combined algorithm therefore offers a more reasonable approach to choose an initial approximation for the IART and improve the quality of the final reconstructed image. A numerical simulation experiment demonstrates that the combined algorithm is more accurate than the GSVD alone or the IART alone for the tomographic inversion of IED. The new method is then applied to perform the inversion of the IED during a magnetically disturbed period on 21 August 2003. Tomographic results show that the main ionospheric effects of this storm over China are as follows: the negative storm phase effect appears in F region, the positive storm phase effect occurs above F region, and meanwhile, some prominent features in the ionospheric structure can be revealed in the ionospheric images, such as the disturbance and mid-latitude trough. The reliability of the new method is also validated by the ionosonde data recorded at Wuhan station.
机译:一种新的算法,即广义奇异值分解(GSVD)和改进的代数重建技术(IART)的组合,提出了本文的图像电离层电子密度(IED)分布。在这种新方法中,GSVD首先用于解决计算机化电离层断层扫描(CIT)系统中的不良问题。然后提供从总电子含量(TEC)测量的估计作为IART所需的初始近似。因此,组合算法提供了更合理的方法来选择IART的初始近似,并提高最终重建图像的质量。数值模拟实验表明,组合算法比单独的GSVD更准确,也可以单独的IART用于IED的断层倒置。然后应用新方法以在2003年8月21日在磁性干扰期间进行IED的反转。断层摄影结果表明,这场风暴对中国的主要电离层效应如下:负暴风阶段效应出现在F地区,同时,在F区域上方发生正风暴相位效应,并且可以在电离层图像中揭示电离层结构中的一些突出特征,例如扰动和中纬度槽。新方法的可靠性也由武汉站记录的Ionosonde数据验证。

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