EVALUATION OF THE S4 SCINTILLATIONS INDEX IN TRANSCONTINENTAL DECAMETER RADIO LINES

V.P. SIVOKON
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Abstract

On the HAARP and EISCAT heating stands, to solve a number of applied problems, studies are being carried out on the excitation of an interlayer ionospheric waveguide. The success of the implementation of these tasks depends on many factors, including the level of fading of the electromagnetic field in the waveguide, to assess the variations of which researchers use the scintillation index S4. The waveguide excitation model proposed by the experimenters is based on the perspective "self-scattering effect" on artificial magnetically oriented irregulars of the ionosphere. However, within the frame work of this approach, the possibility of the existence of other mechanisms of excitation of the waveguide and the influence of the geophysical environment on this process is not taken into account. To test this assumption, we use multi-position diagnostics based on SDR technology. Measurements on quasi-longitudinal and quasi-transverse paths with respect to the Earth's magnetic field line, as well as under different geophysical conditions, showed a significant difference in the variations of the scintillation index S4 and the intensity of the scattered wave. The results obtained can be used in the problems of optimizing schemes for pumping an information signal into an interlayer ionospheric waveguide.
横贯大陆十米无线电线路s4闪烁指数的评价
在HAARP和EISCAT加热台上,为了解决一些应用问题,正在进行层间电离层波导的激发研究。这些任务的成功实施取决于许多因素,包括波导中电磁场的衰落水平,研究人员使用闪烁指数S4来评估其变化。实验人员提出的波导激励模型是基于电离层人工磁定向不规则体的“自散射效应”的观点。然而,在这种方法的框架内,没有考虑到存在其他波导激励机制的可能性以及地球物理环境对这一过程的影响。为了验证这一假设,我们使用了基于SDR技术的多位置诊断。在地球磁力线的准纵向和准横向路径以及不同地球物理条件下的测量结果表明,闪烁指数S4的变化和散射波强度存在显著差异。所得结果可用于电离层间波导中抽运信息信号的优化方案问题。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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