电离层无线电传播中的频率扩展

R. Shepherd, J. Lomax
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引用次数: 44

摘要

作为电离层无线电传播时间和频率色散特性研究项目的一部分,研究人员开发了精确测量接收到的连续波信号功率谱的技术。频率分辨率为0.025 Hz。这种分辨率允许观察各种传播模式,并借助于同时拍摄的斜入射电离图来识别模式。有时,即使是波的普通和特殊成分也能被分离和识别。功率谱是在接近太阳周期最小值的一年时间里,在中纬度路径和经极光路径上进行的测量得出的。除了绘制功率谱外,还计算了谱的均方根宽度(定义为频率扩展)和均值(或平均多普勒频移)。给出了这些数据的分布,并将频率扩展与磁活动、时延扩展和模式数进行了比较。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Frequency Spread in Ionospheric Radio Propagation
As part of a research program on the time- and frequency-dispersive characteristics of ionospheric radio propagation, techniques were developed for precise measurement of the power spectrum of a received CW signal. Frequency resolution of 0.025 Hz is obtained. This resolution allows the observation of the various propagating modes and, with the aid of oblique-incidence ionograms taken simultaneously, identification of the modes. Occasionally, even the ordinary and extraordinary components of the wave can be separated and identified. Power spectra were derived from measurements made on a midlatitude path and on a transauroral path over a period of one year near the solar cycle minimum. In addition to the plotting of the power spectra, the root-mean-square widths of the spectra (defined as the frequency spread) and the means (or average Doppler shift) were computed. Distributions of these data are presented, and the frequency spread is compared with the magnetic activity, the timedelay spread, and the number of modes.
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