On the Possibility of Sounding the Boundaries of the Nothern Auroral Oval by Registrations of High Frequency Signals on Superlong Radio Paths

O. V. Charkin, A. Zalizovski, Y. Yampolski
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Abstract

Objective. Developing a technique for investigation of a dynamic of the equatorial boundary of the night side of the Northern auroral oval using data of registrations of scattered HF signals on superlong radio paths. Methods. Spectral, time, and time-frequency analysis of HF signals from time service stations, recorded at the Ukrainian Antarctic Akademik Vernadsky station (UAS). Selection of the spatial mode of signals scattered on the plasma inhomogeneities of the high latitude ionosphere of the northern hemisphere. The developed method is based on the measurement of the Doppler frequency shift and time of the group delay of the radio signal. Results. The possibility of studying the dynamics of the equatorial boundary of the night side of the Northern auroral oval using characteristics of scattered HF signals of time service stations registered at UAS is demonstrated. Conclusions. In the registrations of HF signals of the RWM station (55.75°N, 37.64°E) at UAS (65.25°S, 64.27°W) it is possible to select the mode scattered on the inhomogeneities of the high-latitude ionosphere of the northern hemisphere. The method for diagnosing the equatorial boundary of the auroral oval by observations on UAS of scattered radio signals from stations of the time service is proposed. It is convenient to use such stations as sources of the probe signal for diagnostic of the ionosphere so far as they have a number of advantages, including low relative frequency instability of master oscillators; weakly directed antennas and sufficiently powerful transmitters thanks to which their signals can be recorded in different regions of the globe; continuous work on a previously known schedule and, finally, the fact that they simultaneously emit at several frequencies, which expands the possibilities of their diagnostic use. The technique does not require additional transmitting devices and expensive antenna systems. The regular measurements using the suggested method allow carrying out the monitoring of auroral ionosphere, which will give the possibility for improving the existent models of its behavior.
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超长无线电路径高频信号配准探测北极光椭圆边界的可能性
目标。发展了一种利用超长无线电路径散射高频信号资料研究北极光椭圆夜侧赤道边界动力学的技术。方法。乌克兰南极维尔纳德斯基科考站(UAS)记录的时间服务站高频信号的频谱、时间和时频分析。北半球高纬度电离层等离子体非均匀性散射信号的空间模式选择。所开发的方法是基于对无线电信号的多普勒频移和群延迟时间的测量。结果。论证了利用UAS授时服务站散射高频信号特征研究北极光椭圆夜侧赤道边界动力学的可能性。结论。RWM站(55.75°N, 37.64°E)在UAS(65.25°S, 64.27°W)的高频信号配准中,可以选择北半球高纬度电离层的非均匀性散射模态。提出了一种利用授时台站散射无线电信号UAS观测诊断极光椭圆赤道边界的方法。利用这些台站作为探测信号源诊断电离层是很方便的,因为它们有许多优点,包括主振荡器的相对频率不稳定性低;弱定向天线和足够强大的发射机,它们的信号可以在全球不同地区被记录下来;按照事先已知的时间表连续工作,最后,它们同时以几个频率发射,这扩大了它们诊断用途的可能性。该技术不需要额外的传输设备和昂贵的天线系统。使用所建议的方法进行的定期测量允许对极光电离层进行监测,这将使改进其行为的现有模型成为可能。
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