On the Spectrum of Geomagnetic Variations Accompanying Jerks

IF 0.9 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
S. A. Riabova, S. L. Shalimov
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引用次数: 0

Abstract—Based on the data of several spaced magnetic stations, the spectrum of geomagnetic variations is studied in the range of periods from two to 40 years. Special attention is paid to spectral features in the supposed range of action of intraterrestrial processes that cause geomagnetic jerks. It is shown that the detected spectral peak in the vicinity of the period of 6.5 years aligns with the previously revealed recurrence pattern of jerks with a period of three to four years; however, this peak is absent in the spectrum of solar activity. The possible wave mechanisms of the occurrence of jerks and their 6-year quasi-periodicity caused by known types of magnetohydrodynamic waves in the liquid core of the Earth, are considered, and it is shown that they are not sufficiently convincing in reproducing observations of jerks.

Abstract Image

关于伴随飓风的地磁变化频谱
摘要 根据几个间隔磁力站的数据,研究了从 2 年到 40 年周期范围内的地磁变化频谱。研究特别关注了造成地磁颠簸的地内过程的假定作用范围内的频谱特征。结果表明,在 6.5 年周期附近检测到的光谱峰值与之前揭示的 3 至 4 年周期的地磁骤变复发模式一致;然而,在太阳活动光谱中却没有这个峰值。研究考虑了地球液态内核中已知类型的磁流体动力波可能引起的跃迁及其 6 年准周期性的波机制,结果表明,这些机制在再现跃迁观测结果方面没有足够的说服力。
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来源期刊
Izvestiya, Physics of the Solid Earth
Izvestiya, Physics of the Solid Earth 地学-地球化学与地球物理
CiteScore
1.60
自引率
30.00%
发文量
60
审稿时长
6-12 weeks
期刊介绍: Izvestiya, Physics of the Solid Earth is an international peer reviewed journal that publishes results of original theoretical and experimental research in relevant areas of the physics of the Earth''s interior and applied geophysics. The journal welcomes manuscripts from all countries in the English or Russian language.
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