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Modeling scattering from lightning-induced ionospheric disturbances with the discontinuous Galerkin method

机译:用不连续Galerkin方法模拟雷电引起的电离层扰动的散射

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Simulation of the propagation of very low frequency (VLF) waves in the Earth-ionosphere waveguide remains a significant computational challenge as a result of the variable wavelength at these frequencies in the magnetized plasma environment of the lower ionosphere. The discontinuous Galerkin (DG) method is naturally and easily adapted to nonuniform grids and so is ideal for simulation in media where the characteristic length scale varies significantly. We present an automatic procedure based on minimal system realization to incorporate any linear, anisotropic dispersive material in the DG framework, with application to a perfectly matched layer and scattering from strong disturbances in a magnetoplasma. We apply these techniques to modeling of scattering from lightning electromagnetic pulse–induced ionospheric disturbances, calculating the full 3-D scattered VLF wavefields from intense lightning-induced ionospheric perturbations over a large volume. We plot the spatial distribution of the phase and amplitude response as seen by a ground-based receiver over a large area. The results are consistent with previous results from 2-D models, showing maximum received signal strength amplitude perturbations on the order of 0.1 to 0.2 dB for intense vertical discharges under smooth ambient conditions and on the order of 0.5 dB for very intense, repeated horizontal discharges.
机译:由于在较低电离层的磁化等离子体环境中,在这些频率下波长可变,因此模拟电离层波导中的甚低频(VLF)波的传播仍然是一项重大的计算挑战。不连续的Galerkin(DG)方法自然而又容易地适用于非均匀网格,因此非常适合在特征长度尺度发生显着变化的介质中进行仿真。我们提出了一个基于最小系统实现的自动程序,该程序将任何线性各向异性分散材料纳入DG框架,并应用于完美匹配的层并从磁等离子体中的强烈干扰中散射。我们将这些技术应用于雷电电磁脉冲引起的电离层扰动的散射建模,并根据大体积雷电引起的电离层扰动来计算完整的3-D散射VLF波场。如地面接收器在大面积上看到的,我们绘制了相位和幅度响应的空间分布。结果与2-D模型的先前结果一致,在平滑的环境条件下,剧烈的垂直放电的最大接收信号强度幅度扰动为0.1到0.2 dB左右,非常强的重复水平放电的最大接收信号强度幅度扰动为0.5 dB左右。

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