The State of Solar Wind Heavy Ions in Interplanetary Coronal Mass Ejection–Driven Geomagnetic Storms

During geomagnetic storms, which are the primary periods for heavy ions from the solar wind to enter Earth’s magnetospheric space, the charge state of solar wind heavy ions during these storms has significant implications for studying the distribution and effects of heavy ions in the magnetosphere....

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Published in:The Astrophysical Journal
Main Authors: Cong Wang, Fei He, Xiaoxin Zhang
Format: Article
Language:English
Published: IOP Publishing 2024-01-01
Subjects:
Online Access:https://doi.org/10.3847/1538-4357/ad7b07
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author Cong Wang
Fei He
Xiaoxin Zhang
author_facet Cong Wang
Fei He
Xiaoxin Zhang
author_sort Cong Wang
collection DOAJ
container_title The Astrophysical Journal
description During geomagnetic storms, which are the primary periods for heavy ions from the solar wind to enter Earth’s magnetospheric space, the charge state of solar wind heavy ions during these storms has significant implications for studying the distribution and effects of heavy ions in the magnetosphere. We analyzed the states and variations of heavy ions during 158 interplanetary coronal mass ejection (ICME)–driven geomagnetic storm events using data from the Advanced Composition Explorer satellite and examined four of these events in detail. We found that the increase in the average charge state of heavy ions such as O, Mg, Si, and Fe is positively correlated with the intensity of the geomagnetic storm. Regarding the abundance ratio of heavy ions such as Ne, Mg, Si, and Fe relative to oxygen ions, the rate and magnitude of increase in abundance ratios during extreme geomagnetic storms ( Kp = 9) triggered by ICME events are significantly higher than those during other levels of geomagnetic storms. Additionally, we observed that although the average charge states of heavy ions such as O and Fe are correlated with the geomagnetic storm intensity induced by ICMEs, there are significant individual differences in the charge state variations of heavy ions.
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spelling doaj-art-6f48464c0de34ec7894271de669b50032025-08-20T02:12:14ZengIOP PublishingThe Astrophysical Journal1538-43572024-01-01975110610.3847/1538-4357/ad7b07The State of Solar Wind Heavy Ions in Interplanetary Coronal Mass Ejection–Driven Geomagnetic StormsCong Wang0https://orcid.org/0000-0001-8111-1156Fei He1https://orcid.org/0000-0003-0542-2686Xiaoxin Zhang2Chinese Academy of Meteorological Sciences , Beijing, People's Republic of China; Key Laboratory of Space Weather, National Satellite Meteorological Center (National Center for Space Weather) , China Meteorological Administration, Beijing, People's Republic of China ; xxzhang@cma.gov.cn; Innovation Center for FengYun Meteorological Satellite (FYSIC) , Beijing, People's Republic of ChinaKey Laboratory of Earth and Planetary Physics, Institute of Geology and Geophysics, Chinese Academy of Sciences , Beijing, People's Republic of China ; hefei@mail.iggcas.ac.cnKey Laboratory of Space Weather, National Satellite Meteorological Center (National Center for Space Weather) , China Meteorological Administration, Beijing, People's Republic of China ; xxzhang@cma.gov.cn; Innovation Center for FengYun Meteorological Satellite (FYSIC) , Beijing, People's Republic of ChinaDuring geomagnetic storms, which are the primary periods for heavy ions from the solar wind to enter Earth’s magnetospheric space, the charge state of solar wind heavy ions during these storms has significant implications for studying the distribution and effects of heavy ions in the magnetosphere. We analyzed the states and variations of heavy ions during 158 interplanetary coronal mass ejection (ICME)–driven geomagnetic storm events using data from the Advanced Composition Explorer satellite and examined four of these events in detail. We found that the increase in the average charge state of heavy ions such as O, Mg, Si, and Fe is positively correlated with the intensity of the geomagnetic storm. Regarding the abundance ratio of heavy ions such as Ne, Mg, Si, and Fe relative to oxygen ions, the rate and magnitude of increase in abundance ratios during extreme geomagnetic storms ( Kp = 9) triggered by ICME events are significantly higher than those during other levels of geomagnetic storms. Additionally, we observed that although the average charge states of heavy ions such as O and Fe are correlated with the geomagnetic storm intensity induced by ICMEs, there are significant individual differences in the charge state variations of heavy ions.https://doi.org/10.3847/1538-4357/ad7b07Solar coronal mass ejectionsSolar windCharge exchange ionizationGeomagnetic fields
spellingShingle Cong Wang
Fei He
Xiaoxin Zhang
The State of Solar Wind Heavy Ions in Interplanetary Coronal Mass Ejection–Driven Geomagnetic Storms
Solar coronal mass ejections
Solar wind
Charge exchange ionization
Geomagnetic fields
title The State of Solar Wind Heavy Ions in Interplanetary Coronal Mass Ejection–Driven Geomagnetic Storms
title_full The State of Solar Wind Heavy Ions in Interplanetary Coronal Mass Ejection–Driven Geomagnetic Storms
title_fullStr The State of Solar Wind Heavy Ions in Interplanetary Coronal Mass Ejection–Driven Geomagnetic Storms
title_full_unstemmed The State of Solar Wind Heavy Ions in Interplanetary Coronal Mass Ejection–Driven Geomagnetic Storms
title_short The State of Solar Wind Heavy Ions in Interplanetary Coronal Mass Ejection–Driven Geomagnetic Storms
title_sort state of solar wind heavy ions in interplanetary coronal mass ejection driven geomagnetic storms
topic Solar coronal mass ejections
Solar wind
Charge exchange ionization
Geomagnetic fields
url https://doi.org/10.3847/1538-4357/ad7b07
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