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Simulation study of the interaction between large-amplitude HF radio waves and the ionosphere

机译:大振幅HF无线电波与电离层相互作用的仿真研究

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The time evolution of a large-amplitude electromagnetic (EM) wave injected vertically into the overhead ionosphere is studied numerically. The EM wave has a carrier frequency of 5 MHz and is modulated as a Gaussian pulse with a width of approximately 0.1 milliseconds and a vacuum amplitude of 1.5 V/m at 50 km. This is a fair representation of a modulated radio wave transmitted from a typical high-power HF broadcast station on the ground. The pulse is propagated through the neutral atmosphere to the critical points of the ionosphere, where the L-O and R-X modes are reflected, and back to the neutral atmosphere. We observe mode conversion of the L-O mode to electrostatic waves, as well as harmonic generation at the turning points of both the R-X and L-O modes, where their amplitudes rise to several times the original ones. The study has relevance for ionospheric interaction experiments in combination with ground-based and satellite or rocket observations.
机译:数值研究了垂直注入高架电离层的大振幅电磁波的时间演化。 EM波的载波频率为5 MHz,在50 km处被调制为高斯脉冲,其宽度约为0.1毫秒,真空幅度为1.5 V / m。这是从地面上典型的高功率HF广播电台发射的调制无线电波的合理表示。脉冲通过中性大气传播到电离层的临界点,在该点上,L-O和R-X模式被反射,然后返回中性大气。我们观察到从L-O模式到静电波的模式转换,以及在R-X和L-O模式转折点处的谐波生成,它们的振幅上升到原始振幅的几倍。该研究与电离层相互作用实验以及地面,卫星或火箭观测相结合具有重要意义。

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