赤道电射流的极性振荡对 2023 年 12 月 1 日地磁风暴的响应

IF 2.6 2区 地球科学 Q2 ASTRONOMY & ASTROPHYSICS
Kedeng Zhang, Hui Wang, Huimin Song
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引用次数: 0

摘要

2023 年 12 月 1 日的中度地磁暴非常有趣,北京出乎意料地观测到了极光。在这场风暴中,赤道电射流(EEJ)的行为可能值得探讨。当昼间电场的极化向西变化时,EEJ 的方向也会向西,这就是所谓的逆电射流(CEJ)。利用全球导航卫星系统的总电子含量、Tatuoca 站和低轨道 Swarm 卫星观测到的 EEJ 以及热层-电离层电动大气环流模式的相应模拟,探讨了 2023 年 12 月 1 日地磁风暴期间 EEJ 响应的极化振荡(ΔEEJ)。在当地时间(LT)9 点 6 分和 12 点 8 分,观测到的 Swarm ΔEEJ 出现了明显的极化振荡。在当地时间 15 时也发现了类似的振荡。ΔEEJ 的强烈极性振荡由电场主导,电离层考林电导率的影响可忽略不计。ΔEEJ与电场变化(ΔE)之间的相关系数大于0.87,证实了电场的作用。在午前扇区,ΔEEEJ 的准振荡受中性风和快速穿透电场(PPEF)的控制。正午时,ΔEEEJ 主要由 PPEF 驱动,中性风的影响较小。在下午,ΔEEJ 主要由 PPEF 驱动,中性风的影响可忽略不计。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Polarity Oscillations of the Equatorial Electrojet in Response to the Geomagnetic Storm on 1 December 2023

The moderate geomagnetic storm on 1 December 2023 is interesting that the aurora is unexpectedly observed in Beijing. During this storm, the behaviors of the equatorial electrojet (EEJ) might deserve to be explored. When the polarization of the daytime electric field changes westward, the direction of EEJ turns westward as well, termed the counter electrojet (CEJ). Using the total electron content from Global Navigation Satellite System, observed EEJ from Tatuoca station and low-orbit Swarm satellites, and the corresponding simulations from the Thermosphere-Ionosphere Electrodynamic General Circulation Model, the polarization oscillations of EEJ responses (ΔEEJ) during the geomagnetic storm on 1 December 2023 are explored. A significant polarity oscillation is established in the Swarm-observed ΔEEJ at 9.6 and 12.8 local time (LT). A similar oscillation is also found at 15 LT. The strong polarity oscillations of ΔEEJ are dominated by the electric field, with ignorable effects from the ionospheric Cowling conductivity. The correlation coefficient between ΔEEJ and electric field changes (ΔE) is larger than 0.87, confirming the roles of the electric field. In the pre-noon sector, the quasi-oscillations of ΔEEJ are controlled by both the neutral winds and the prompt penetration electric field (PPEF). At noon, ΔEEJ is primarily driven by the PPEF, with minor effects from neutral winds. At afternoon, ΔEEJ is attributed to the PPEF, and the effects of neutral winds are ignorable.

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来源期刊
Journal of Geophysical Research: Space Physics
Journal of Geophysical Research: Space Physics Earth and Planetary Sciences-Geophysics
CiteScore
5.30
自引率
35.70%
发文量
570
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