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Titlebook: ELF-VLF Radio Wave Propagation; Proceedings of the N Jan A. Holtet Conference proceedings 1974 Springer Science+Business Media Dordrecht 19

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樓主: 大破壞
41#
發(fā)表于 2025-3-28 17:53:42 | 只看該作者
42#
發(fā)表于 2025-3-28 20:59:26 | 只看該作者
43#
發(fā)表于 2025-3-29 02:12:39 | 只看該作者
LCM Laboratorio de la Ciudad de Mexico,tion may be significant during disturbed conditions such as a PCA or auroral absorption event. Cole and Pierce (1965) found that the dominant influence changes from electrons above to ions below at about 50 km altitude.
44#
發(fā)表于 2025-3-29 03:27:33 | 只看該作者
he principal reason being that the attenuation of the waves is very low and the phase stability of the waves is very high. Thus, these waves find numerous applications in global communications and in long-range navigation systems.
45#
發(fā)表于 2025-3-29 09:18:29 | 只看該作者
46#
發(fā)表于 2025-3-29 15:03:41 | 只看該作者
The Photochemistry of the Mesospherer ions in the D-region. If we therefore know the abundance of these species, their diurnal and seasonal variations, and also possible variations with the solar cycle, we might be able to explain some of the discrepancies which are obtained in measurements performed under different atmospheric condit
47#
發(fā)表于 2025-3-29 17:03:20 | 只看該作者
Theory of Energy Flux and Polarisation Changes of a Radio Wave with Two Magnetoionic Components Undee is reduced. This is called ‘self-demodulation’, and is the main subject of this discussion. If the power of the disturbing wave is very large, ‘self-demodulation’ is accompanied by ‘self-distortion’ effects because of the large change in collision frequency distorting the original wave form of the
48#
發(fā)表于 2025-3-29 20:34:49 | 只看該作者
49#
發(fā)表于 2025-3-30 02:01:26 | 只看該作者
50#
發(fā)表于 2025-3-30 04:52:07 | 只看該作者
Nazi Massacres and Divided Memory,r ions in the D-region. If we therefore know the abundance of these species, their diurnal and seasonal variations, and also possible variations with the solar cycle, we might be able to explain some of the discrepancies which are obtained in measurements performed under different atmospheric condit
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