Investigating Topside Ionospheric Responses to the November 2003 Superstorm Using CHAMP, GRACE, and SAC-C Satellite Observations

IF 2.6 2区 地球科学 Q2 ASTRONOMY & ASTROPHYSICS
Hailun Ye, Wen Yi, Jianfei Wu, Bingkun Yu, Jiahao Zhong, Xianghui Xue, Penghao Tian, Chi Long, Jian Li, Maolin Lu, Chong Wang, Tingdi Chen, Xiankang Dou
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Abstract

In this work, topside Total Electron Content (TEC) obtained from CHAMP, GRACE, and SAC-C, along with in situ electron density (Ne) measurements from CHAMP and GRACE, were utilized to investigate the response of the topside ionosphere to the November 2003 superstorm, particularly during its recovery phase. Observations from multiple satellites revealed unexpected and persistent enhancements in the topside ionosphere during the late recovery phase (22–24 November 2003), which were more pronounced in the Eastern Pacific sector than in the Asian sector, indicating notable longitudinal differences. Intriguingly, the opposite inter-hemispheric asymmetries of the enhancement were observed near the peak height of F2 and the topside ionosphere on the dayside in the Eastern Pacific sector. During the late recovery phase, the storm-time enhancement in the eastward electric field and trans-equatorial wind likely contributed to the observed positive ionospheric storm effects and inter-hemispheric asymmetry, respectively. Additionally, this study confirmed substantial enhancements in the dayside topside ionosphere during the storm's main phase on 20 November 2003. These findings underscore the need for a global, multi-instrumental approach to fully understand the diverse responses of the topside ionosphere to geomagnetic storms.

利用CHAMP、GRACE和SAC-C卫星观测研究2003年11月超级风暴对上层电离层的响应
在这项工作中,利用CHAMP、GRACE和SAC-C获得的上层总电子含量(TEC),以及CHAMP和GRACE的原位电子密度(Ne)测量结果,研究了上层电离层对2003年11月超级风暴的响应,特别是在它的恢复阶段。多颗卫星的观测显示,在恢复后期(2003年11月22日至24日),上层电离层出乎意料地持续增强,这种增强在东太平洋区域比在亚洲区域更为明显,表明显著的纵向差异。有趣的是,在F2峰高度附近和东太平洋区域日侧电离层顶部观测到相反的半球间不对称增强。在恢复后期,东部电场和跨赤道风的风暴时间增强可能分别导致了观测到的电离层正风暴效应和半球间不对称。此外,这项研究证实了在2003年11月20日风暴主要阶段白天上层电离层的显著增强。这些发现强调需要一个全球性的、多仪器的方法来充分了解上层电离层对地磁风暴的不同响应。
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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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