Multiple-Band Electric Field Response to the Geomagnetic Storm on 4 November 2021

被引:0
|
作者
Zheng, Jie [1 ,2 ]
Huang, Jianping [2 ]
Li, Zhong [3 ]
Li, Wenjing [2 ]
Han, Ying [3 ]
Lu, Hengxin [2 ]
Zhima, Zeren [2 ]
机构
[1] Univ Chinese Acad Sci, Beijing 101408, Peoples R China
[2] Minist Emergency Management China, Natl Inst Nat Hazards, Beijing 100085, Peoples R China
[3] Inst Disaster Prevent, Langfang 065201, Peoples R China
关键词
CSES; electric field disturbance; geomagnetic storms; ULF; ELF; VLF; HF; ULF INDEX; PULSATIONS; SUBSTORMS;
D O I
10.3390/rs16183497
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
This paper investigates the impact characteristics of the 4 November 2021 magnetic storm across different frequency bands based on the electric field data (EFD) from the China Seismo-Electromagnetic Satellite (CSES), categorized into four frequency bands: ULF (Ultra-Low-Frequency, DC to 16 Hz), ELF (Extremely Low-Frequency, 6 Hz to 2.2 kHz), VLF (Very Low-Frequency, 1.8 to 20 kHz), and HF (High-Frequency, 18 kHz to 3.5 MHz). The study reveals that in the ULF band, magnetic storm-induced electric field disturbances are primarily in the range of 0 to 5 Hz, with a significant disturbance frequency at 3.9 +/- 1.0 Hz. Magnetic storms also enhance Schumann waves in the ULF band, with 8 Hz Schumann waves dominating in the southern hemisphere and 13 Hz Schumann waves dominating in the northern hemisphere. In the ELF band, the more pronounced anomalies occur at 300 Hz-900 Hz and above 1.8 kHz, with the 300 Hz-900 Hz band anomalies around 780 Hz being the most significant. In the VLF band, the electric field anomalies are mainly concentrated in the 3-15 kHz range. The ELF and VLF bands exhibit lower absolute and relative disturbance increments compared to the ULF band, with the relative perturbation growth rate in the ULF band being approximately 10% higher than in the ELF and VLF bands. Magnetic storm-induced electric field disturbances predominantly occur in the ULF, ELF, and VLF bands, with the most significant disturbances in the ULF band. The electric field perturbations in these three frequency bands exhibit hemispheric asymmetry, with strong perturbations in the northern hemisphere occurring earlier than in the southern hemisphere, corresponding to different Dst minima. No electric field disturbances were observed in the HF band (above 18 kHz). The conclusions of this paper are highly significant for future anti-jamming designs in spacecraft and communication equipment, as well as for the further study of magnetic storms.
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页数:22
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