夜侧磁层地磁脉动谱中特征频率群的结构

A. Polyakov
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引用次数: 0

摘要

利用一种新的振幅和相位波动相关函数(APCF)方法,对夜侧磁层若干小时区的地磁场分量波动记录进行了处理(观测站monday和Borok)。该方法旨在检测源信号频谱内的等距离频率组,并测量这些组中每个组中两个相邻频率之间的差异。这些波动的宽带频谱中的等距频率群与白天波动一样,取决于二维alfvsamn波谐振器的特征频率[Polyakov, 2018]。该谐振器的参数组合与当地时间之间存在经验关系。在几乎所有时带的alfvsamn波动N-S和E-W分量处理的最终产品中,结构元件之间的相似性清楚地表明APCF方法处理任何宽带信号的结果的可靠性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Structure of groups of eigenfrequencies in spectra of geomagnetic pulsations in the nightside magnetosphere
Using a new method of correlation function for amplitude and phase fluctuations (APCF), records of geomagnetic field component fluctuations (observatories Mondy and Borok) have been processed for a number of hour zones of the nightside magnetosphere. This method is meant to detect groups of equidistant frequencies inside the spectrum of source signal and also to measure a difference between two neighbor frequencies in each of these groups. The groups of equidistant frequencies in broadband spectra of these fluctuations are shown to depend on eigenfrequencies of the 2D Alfvén wave resonator, just as for dayside fluctuations [Polyakov, 2018]. An empirical relation has been found between a combination of parameters of this resonator and local time. The similarity between structural elements in the final products of processing of Alfvén fluctuation N-S and E-W components for almost all hour zones clearly indicates the reliability of the results of the APCF method in processing any broadband signals.
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