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引用次数: 0
摘要
本文研究了磁层中产生的极低频电磁波(即Pc2-Pc5微脉动)的傅里叶谱频率最大值F和最大值在(F = 7-50) MHz频段内的特性。它应被视为论文II (Alpert et al., 1995)中提出的数据分析的扩展部分。将所得的谱特征与能模拟未滤波磁场B(t)检测记录包络形状的信号谱进行了比较。它们还面临着不同信号的频谱频率最大值和不同谐振器的共振频率。这一分析证实了我们的结论,即所发现的频谱最大值可以是磁层振荡系统的共振频率特征值。通过简单的计算,模拟了背景等离子体振荡的共振摆动,产生了强波包。在磁层中观测到的经过过滤的波包的形状的变化是通过这些计算得到的。
Oscillatory Nature of the Magnetosphere III. Resonance Oscillations. Some Simulation
The characteristics of the Fourier spectral frequency maxima Fs, max in the frequency band (F = 7-50) MHz which compose the extra low frequency e.m. waves-so called Pc2-Pc5 micropulsations, created in the magnetosphere are considered in this paper. It should be considered as an extended part of the data analysis presented in paper II (Alpert et al., 1995). The obtained characteristics of the spectra are compared with spectra of signals which can simulate the shapes of the envelopes of the examined records of the unfiltered magnetic field B(t). They are also confronted with spectral frequency maxima of different signals and with resonance frequencies of different resonators. This analysis confirms our conclusion that the found spectral maxima can be resonance frequencies-eigenvalues of a magnetospheric oscillating system. The resonance swinging of the background plasma oscillations, which creates strong packets of waves is also simulated by simple calculations. The variety, of shapes of the filtered packets of waves as observed in the magnetosphere is obtained by these calculations.