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The effect of subionospheric propagation on whistlers recorded by the DEMETER satellite - observation and modelling

机译:亚电离层传播对DEMETER卫星记录的口哨声的影响-观测与建模

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摘要

During a routine analysis of whistlers on the wideband VLF recording of the DEMETER satellite, a specific signal structure of numerous fractional-hop whistlers, termed the "Spiky Whistler" (SpW) was identified. These signals appear to be composed of a conventional whistler combined by the compound mode-patterns of guided wave propagation, suggesting a whistler excited by a lightning "tweek" spheric. Rigorous, full-wave modelling of tweeks, formed by the long subionospheric guided spheric propagation and of the impulse propagation across an arbitrarily inhomoge-neous ionosphere, gave an accurate description of the SpW signals. The electromagnetic impulses excited by vertical, preferably CG lightning discharge, exhibited the effects of guided behaviour and of the dispersive ionospheric plasma along their paths. This modelling and interpretation provides a consistent way to determine the generation and propagation characteristics of the recorded SpW signals, as well as to describe the traversed medium.
机译:在对DEMETER卫星的宽带VLF记录上的哨声进行例行分析期间,确定了许多分数跳哨声的特定信号结构,称为“尖啸声”(SpW)。这些信号似乎由常规的啸叫声和引导波传播的复合模式组合而成,表明啸叫声被闪电的“ tweek”球激发。由长时间的电离层引导的球形传播和任意非均匀电离层的脉冲传播形成的对tweeks的严格全波建模,对SpW信号进行了精确描述。垂直,最好是CG闪电放电激发的电磁脉冲沿其路径表现出引导行为和电离层等离子体的行为。这种建模和解释提供了确定记录的SpW信号的生成和传播特性以及描述所遍历介质的一致方法。

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