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An improved ray theory and transfer matrix method-based model for lightning electromagnetic pulses propagating in Earth-ionosphere waveguide and its applications

机译:改进的基于射线理论和传递矩阵法的地球电离层波导中传播的雷电电磁脉冲模型及其应用

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摘要

An improved ray theory and transfer matrix method-based model for a lightning electromagnetic pulse (LEMP) propagating in Earth-ionosphere waveguide (EIWG) is proposed and tested. The model involves the presentation of a lightning source, parameterization of the lower ionosphere, derivation of a transfer function representing all effects of EIWG on LEMP sky wave, and determination of attenuation mode of the LEMP ground wave. The lightning source is simplified as an electric point dipole standing on Earth surface with finite conductance. The transfer function for the sky wave is derived based on ray theory and transfer matrix method. The attenuation mode for the ground wave is solved from Fock's diffraction equations. The model is then applied to several lightning sferics observed in central China during day and night times within 1000 km. The results show that the model can precisely predict the time domain sky wave for all these observed lightning sferics. Both simulations and observations show that the lightning sferics in nighttime has a more complicated waveform than in daytime. Particularly, when a LEMP propagates from east to west (Phi = 270 degrees) and in nighttime, its sky wave tends to be a double-peak waveform (dispersed sky wave) rather than a single peak one. Such a dispersed sky wave in nighttime may be attributed to the magneto-ionic splitting phenomenon in the lower ionosphere. The model provides us an efficient way for retrieving the electron density profile of the lower ionosphere and hence to monitor its spatial and temporal variations via lightning sferics.
机译:提出并测试了基于改进的射线理论和传递矩阵方法的地球电离层波导(EIWG)中传播的雷电电磁脉冲(LEMP)模型。该模型涉及雷电的呈现,下部电离层的参数化,代表EIWG对LEMP天波的所有影响的传递函数的推导以及LEMP地波衰减模式的确定。闪电源简化为以有限电导率站立在地球表面的电偶极子。基于射线理论和传递矩阵法推导了天波的传递函数。地面波的衰减模式由Fock的衍射方程求解。然后将该模型应用于中国中部在1000公里以内的白天和黑夜中观察到的几种雷电。结果表明,该模型可以精确地预测所有这些观测到的雷电特征的时域天波。仿真和观察结果均表明,夜间的雷电特征波形比白天更复杂。特别是,当LEMP从东向西传播(Φ= 270度)并且在夜间传播时,其天波往往是双峰波形(分散的天波),而不是单峰。这种夜间分散的天波可归因于下部电离层中的磁离子分裂现象。该模型为我们提供了一种检索下电离层电子密度分布的有效方法,从而可以通过雷电学来监测其电离时空变化。

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