2022年1月15日汤加火山爆发引起的全球地磁场变化

Pub Date : 2023-08-09 DOI:10.15407/knit2023.04.078
L. F. Chernogor
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引用次数: 0

摘要

汤加火山于2022年1月15日爆发,导致地球(岩石圈、世界海洋)-大气-电离层-磁层系统发生重大紊乱。本文的目的是介绍2022年1月15日汤加火山爆发引起的全球地磁场变化的研究结果。为了分析地磁场的X、Y和z分量的变化,使用了全球INTERMAGNET网络12个站点的注册资料。在处理时间序列时,首先减去步长为1 min的60 min以内的趋势,然后进行系统谱分析。对空间天气状况的分析使得选择2022年1月13日和17日作为参考日成为可能。对地磁场各分量水平的时间变化的分析显示如下。在火山爆发当天,大约在04:21之后,所有分量的水平都发生了显著变化,但y分量的水平变化最大。同时,火山爆发产生的驻声波场的声共振引起了周期为4 ~ 4.5 min、振幅为~ 2nt的地磁场准周期变化。此外,还发现了六组可能由火山爆发引起的扰动。重要的是,在每一组中,干扰的时间延迟随着火山与观测站之间距离的增加而增加。结果表明,扰动的传输速度分别接近4、1.5、1 km/s和500、313、200 m/s。这种速度是慢MHD波、爆炸波、大气重力波、兰姆波和电离层海啸波的特征。
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GLOBAL VARIATIONS IN THE GEOMAGNETIC FIELD CAUSED BY THE EXPLOSION OF THE TONGA VOLCANO ON JANUARY 15, 2022
The explosion of the Tonga volcano on January 15, 2022, led to significant disturbances in the Earth (lithosphere, World Ocean) — atmosphere — ionosphere — magnetosphere system. The purpose of this paper is to present the results of a study of global variations in the geomagnetic field caused by the explosion of the Tonga volcano on January 15, 2022. To analyze the variations of the X-, Y-, and Z-components of the geomagnetic field, registrations at 12 stations of the worldwide INTERMAGNET network were used. When processing the time series, the trend calculated over 60 min with a step of 1 min was first subtracted, and then a system spectral analysis was applied. An analysis of the state of space weather made it possible to choose January 13 and 17, 2022, as reference days. An analysis of time variations in the level of all components of the geomagnetic field showed the following. On the day of the volcano explosion, approximately after 04:21, there were significant variations in the level of all components, but the largest variations were observed in the level of the Y-component. The shortest time delay was 6 min. At the same time, quasi-periodic variations of the geomagnetic field with a period of 4…4.5 min and an amplitude of ~2 nT were caused by acoustic resonance in the field of a standing acoustic wave generated by the explosion of the volcano. In addition, six groups of possible disturbances stimulated by the volcano explosion were found. It is important that in each group, the time delay of disturbances increased with increasing distance between the volcano and the station. It was found that the disturbances were transported at speeds close to 4, 1.5, 1 km/s and 500, 313, and 200 m/s. Such velocities are characteristic of slow MHD waves, a blast wave, an atmospheric gravity wave, a Lamb wave, and an ionospheric tsunami wave.
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