Electromagnetic ULF/ELF oscillations caused by the eruption of the Tonga volcano

Pub Date : 2023-03-28 DOI:10.12737/stp-91202306
V. Martines-Bedenko, V. Pilipenko, K. Shiokawa, R. Akbashev
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引用次数: 1

Abstract

The eruption of the Tonga volcano on January 13 and 15, 2022 and related intense lightning activity led to the excitation of a number of specific electromagnetic oscillations in different frequency ranges. We examine properties of these oscillations, using data from magnetometers of various types located in Kamchatka and in the Pacific region. We confirmed that there might have been a geomagnetic response to the formation of an acoustic resonance between the Earth surface and the ionosphere: localized harmonic oscillations with a frequency 3.5–4.0 mHz, which lasted for ~1.5 hr, were detected ~15 min after the beginning of the eruption at distance of ~800 km. An increase was observed in the intensity of the Schumann resonance at stations in the Far East. Broadband emission stimulated by intense volcanic lightning was detected to occur in the Pc1 range (2–5 Hz). The emission presumably results from the excitation of the magnetosonic waveguide in the upper ionosphere by lightning activity.
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汤加火山喷发引起的电磁极低频振荡
2022年1月13日和15日汤加火山爆发以及相关的强烈闪电活动导致了不同频率范围内的一些特定电磁振荡的激发。我们利用堪察加半岛和太平洋地区各种类型的磁力计的数据,研究了这些振荡的性质。我们证实,地球表面和电离层之间的声学共振形成可能有地磁反应:在喷发开始约15分钟后,在约800公里的距离处检测到频率为3.5–4.0 mHz的局部谐波振荡,持续约1.5小时。在远东的台站观测到舒曼共振的强度增加。强烈火山闪电刺激的宽带发射被检测到发生在Pc1范围内(2-5 Hz)。这种发射可能是由于闪电活动对电离层上部磁声波波导的激发。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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