Quantitative analysis of nighttime effects of radiation belt energetic electron precipitation on the D-region ionosphere during lower solar activity periods

<p>Energetic electron precipitation (EEP) from the Earth's radiation belts can ionize neutral molecules in the D-region ionosphere (60–90 km altitude), significantly influencing the conductivity and chemical species therein. However, due to the limited resolution of space-borne instrument...

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Main Authors: X. Dong, S. Zhao, L. Liao, W. Xu, R. Lin, X. Sun, S. Huang, Y. Cui, J. Li, H. Lu, X. Shen
Format: Article
Language:English
Published: Copernicus Publications 2025-08-01
Series:Atmospheric Chemistry and Physics
Online Access:https://acp.copernicus.org/articles/25/9183/2025/acp-25-9183-2025.pdf
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author X. Dong
X. Dong
X. Dong
S. Zhao
S. Zhao
S. Zhao
L. Liao
W. Xu
R. Lin
R. Lin
R. Lin
X. Sun
S. Huang
S. Huang
S. Huang
Y. Cui
Y. Cui
J. Li
J. Li
J. Li
H. Lu
X. Shen
X. Shen
X. Shen
author_facet X. Dong
X. Dong
X. Dong
S. Zhao
S. Zhao
S. Zhao
L. Liao
W. Xu
R. Lin
R. Lin
R. Lin
X. Sun
S. Huang
S. Huang
S. Huang
Y. Cui
Y. Cui
J. Li
J. Li
J. Li
H. Lu
X. Shen
X. Shen
X. Shen
author_sort X. Dong
collection DOAJ
description <p>Energetic electron precipitation (EEP) from the Earth's radiation belts can ionize neutral molecules in the D-region ionosphere (60–90 km altitude), significantly influencing the conductivity and chemical species therein. However, due to the limited resolution of space-borne instruments, the energy and fluxes of electrons that truly precipitate into the atmosphere still remain poorly investigated. To resolve this problem, in this study, we have utilized the wave and particle data measured by the Electric Field Detector (EFD) and High-Energy Particle Detector (HEPP) on board the China Seismo-Electromagnetic Satellite (CSES-01) during nighttime conditions between 2019 and 2021. Using the measurements of extremely low frequency (ELF) waves, we have derived the reflection height of the D-region ionosphere, which turn out to be highly consistent with the electron and X-ray measurements of the CSES. Our results show that the influence of EEP on the two hemispheres is asymmetric: the reflection height in the Northern Hemisphere is in general lowered by 2.5 km, while that in the Southern Hemisphere is lowered by 1.5 km, both of which are consistent with first-principles chemical simulations. We have also found that the decrease in reflection height exhibits strong seasonal variation, which appears to be stronger during wintertime and relatively weaker during summertime. This seasonal difference is likely related to the variation of the background ionospheric electron density. Our findings provide a quantitative understanding of how EEP influences the lower ionosphere during solar minimum periods, which is critical for understanding the magnetosphere–ionosphere coupling and assessing the impact on radio wave propagation.</p>
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spelling doaj-art-814fdb16e6df4d6a91e84791a851d9e72025-08-25T04:55:19ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242025-08-01259183919810.5194/acp-25-9183-2025Quantitative analysis of nighttime effects of radiation belt energetic electron precipitation on the D-region ionosphere during lower solar activity periodsX. Dong0X. Dong1X. Dong2S. Zhao3S. Zhao4S. Zhao5L. Liao6W. Xu7R. Lin8R. Lin9R. Lin10X. Sun11S. Huang12S. Huang13S. Huang14Y. Cui15Y. Cui16J. Li17J. Li18J. Li19H. Lu20X. Shen21X. Shen22X. Shen23State Key Laboratory of Space Weather, National Space Science Center, CAS, Beijing, 100190, ChinaKey Laboratory of Solar Activity and Space Weather, National Space Science Center, CAS, Beijing, 100190, ChinaUniversity of Chinese Academy of Sciences, Beijing, 100190, ChinaState Key Laboratory of Space Weather, National Space Science Center, CAS, Beijing, 100190, ChinaKey Laboratory of Solar Activity and Space Weather, National Space Science Center, CAS, Beijing, 100190, ChinaUniversity of Chinese Academy of Sciences, Beijing, 100190, ChinaInstitute of Geophysics, China Earthquake Administration, Beijing, 100081, ChinaDepartment of Space Physics, School of Electronic Information, Wuhan University, Wuhan, 430072, ChinaState Key Laboratory of Space Weather, National Space Science Center, CAS, Beijing, 100190, ChinaKey Laboratory of Solar Activity and Space Weather, National Space Science Center, CAS, Beijing, 100190, ChinaUniversity of Chinese Academy of Sciences, Beijing, 100190, ChinaInternational Institute for Interdisciplinary and Frontiers, Beihang University, Beijing, ChinaState Key Laboratory of Space Weather, National Space Science Center, CAS, Beijing, 100190, ChinaKey Laboratory of Solar Activity and Space Weather, National Space Science Center, CAS, Beijing, 100190, ChinaUniversity of Chinese Academy of Sciences, Beijing, 100190, ChinaState Key Laboratory of Space Weather, National Space Science Center, CAS, Beijing, 100190, ChinaKey Laboratory of Solar Activity and Space Weather, National Space Science Center, CAS, Beijing, 100190, ChinaState Key Laboratory of Space Weather, National Space Science Center, CAS, Beijing, 100190, ChinaKey Laboratory of Solar Activity and Space Weather, National Space Science Center, CAS, Beijing, 100190, ChinaSchool of Geophysics and Information Technology, China University of Geosciences, Beijing, 100083, ChinaNational Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing, 100085, ChinaState Key Laboratory of Space Weather, National Space Science Center, CAS, Beijing, 100190, ChinaKey Laboratory of Solar Activity and Space Weather, National Space Science Center, CAS, Beijing, 100190, ChinaUniversity of Chinese Academy of Sciences, Beijing, 100190, China<p>Energetic electron precipitation (EEP) from the Earth's radiation belts can ionize neutral molecules in the D-region ionosphere (60–90 km altitude), significantly influencing the conductivity and chemical species therein. However, due to the limited resolution of space-borne instruments, the energy and fluxes of electrons that truly precipitate into the atmosphere still remain poorly investigated. To resolve this problem, in this study, we have utilized the wave and particle data measured by the Electric Field Detector (EFD) and High-Energy Particle Detector (HEPP) on board the China Seismo-Electromagnetic Satellite (CSES-01) during nighttime conditions between 2019 and 2021. Using the measurements of extremely low frequency (ELF) waves, we have derived the reflection height of the D-region ionosphere, which turn out to be highly consistent with the electron and X-ray measurements of the CSES. Our results show that the influence of EEP on the two hemispheres is asymmetric: the reflection height in the Northern Hemisphere is in general lowered by 2.5 km, while that in the Southern Hemisphere is lowered by 1.5 km, both of which are consistent with first-principles chemical simulations. We have also found that the decrease in reflection height exhibits strong seasonal variation, which appears to be stronger during wintertime and relatively weaker during summertime. This seasonal difference is likely related to the variation of the background ionospheric electron density. Our findings provide a quantitative understanding of how EEP influences the lower ionosphere during solar minimum periods, which is critical for understanding the magnetosphere–ionosphere coupling and assessing the impact on radio wave propagation.</p>https://acp.copernicus.org/articles/25/9183/2025/acp-25-9183-2025.pdf
spellingShingle X. Dong
X. Dong
X. Dong
S. Zhao
S. Zhao
S. Zhao
L. Liao
W. Xu
R. Lin
R. Lin
R. Lin
X. Sun
S. Huang
S. Huang
S. Huang
Y. Cui
Y. Cui
J. Li
J. Li
J. Li
H. Lu
X. Shen
X. Shen
X. Shen
Quantitative analysis of nighttime effects of radiation belt energetic electron precipitation on the D-region ionosphere during lower solar activity periods
Atmospheric Chemistry and Physics
title Quantitative analysis of nighttime effects of radiation belt energetic electron precipitation on the D-region ionosphere during lower solar activity periods
title_full Quantitative analysis of nighttime effects of radiation belt energetic electron precipitation on the D-region ionosphere during lower solar activity periods
title_fullStr Quantitative analysis of nighttime effects of radiation belt energetic electron precipitation on the D-region ionosphere during lower solar activity periods
title_full_unstemmed Quantitative analysis of nighttime effects of radiation belt energetic electron precipitation on the D-region ionosphere during lower solar activity periods
title_short Quantitative analysis of nighttime effects of radiation belt energetic electron precipitation on the D-region ionosphere during lower solar activity periods
title_sort quantitative analysis of nighttime effects of radiation belt energetic electron precipitation on the d region ionosphere during lower solar activity periods
url https://acp.copernicus.org/articles/25/9183/2025/acp-25-9183-2025.pdf
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