首页> 外文会议>2019 Russian Open Conference on Radio Wave Propagation >Ionospheric Total Electron Content Derived from GNSS Signals by Double Thin-Shell Model near the Magnetic Equator and Implication in the Meridional Wind
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Ionospheric Total Electron Content Derived from GNSS Signals by Double Thin-Shell Model near the Magnetic Equator and Implication in the Meridional Wind

机译:电磁赤道附近双薄壳模型从GNSS信号推导出的电离层总电子含量及其对子午风的影响

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摘要

A new technique was developed to estimate ionospheric total electron content (TEC) from GNSS satellite signals. The technique is based on the double thin-layer approximation of the ionosphere, i.e., the vertically distributed electron density is parameterized by two thin-shell layers. Total electron content (strictly speaking, partial electron content) associated with each shell is approximated by the functional fitting of spherical surface harmonics. The technique was applied to the dataset obtained by the meridional receiver network in the equatorial Southeast Asia. Characteristics of TEC distribution for the higher and lower layer exhibited different patterns. The north-south symmetry/asymmetry characteristics changed with the local time and layer. These features were ascribed to the thermospheric wind dynamics.
机译:开发了一种从GNSS卫星信号估算电离层总电子含量(TEC)的新技术。该技术基于电离层的双重薄层近似,即垂直分布的电子密度由两个薄壳层参数化。与每个壳相关的总电子含量(严格地说是部分电子含量)可以通过球面谐波的函数拟合来近似。该技术已应用于赤道东南亚经络接收器网络获得的数据集。上层和下层的TEC分布特征表现出不同的模式。南北对称/不对称特征随当地时间和层而变化。这些特征归因于热层风动力学。

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