VLF脉冲在地球-电离层波导中的传播和到达时间

S. Marcus, Eran Greenberg, A. Epstein
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引用次数: 1

摘要

甚低频(VLF)在地球电离层波导中的传播已经引起了人们几十年的兴趣。大多数计算能力都是针对单一频率进行的,通过在频谱上对这些单频分量进行反傅里叶变换,获得与时间相关的结果(例如闪电)。但是,如果对波脉冲的到达时间(TOA)感兴趣,则可以采用计算量较小的方法。由于波导中的单个谱场分量可以表示为模态场的和,并且由于每个模式的群速度不同,因此只需计算群速度最大的模式-最低阶模式即可获得TOA信息。这一原理在一个简单的波导上进行了详细的论证,并应用于地球电离层波导。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Propagation and Time-of-Arrival of VLF Pulses in the Earth-Ionosphere Waveguide
Very low frequency (VLF) propagation in the earth-ionosphere waveguide has been of interest for many decades. Most computational capabilities have been performed for a single frequency, with time-dependent results (such as those applied to lightning) obtained by inverse-Fourier-transforming these single-frequency components over a spectrum of frequencies. But if time-of-arrival (TOA) of a wave pulse is of interest, a less computationally-intensive method can be employed. Since a single spectral field component in the waveguide may be represented as a sum of modal fields, and since the group velocity is different for each mode, only the mode with the largest group velocity – the lowest order mode – need be calculated to obtain TOA information. This principle is demonstrated in detail for a simple waveguide, and applied to the earth-ionosphere waveguide.
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