Geomagnetic Storm Effects on the LEO Proton Flux During Solar Energetic Particle Events

Abstract During a few solar energetic particle (SEP) events, solar protons were trapped within the geomagnetic field and reached the outer edge of the inner radiation belt. We reproduced this phenomenon by modeling the proton flux distribution at the Low‐Earth Orbit (LEO) for different geomagnetic c...

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Main Authors: Kirolosse M. Girgis, Tohru Hada, Akimasa Yoshikawa, Shuichi Matsukiyo, Viviane Pierrard, Susan W. Samwel
Format: Article
Language:English
Published: Wiley 2023-12-01
Series:Space Weather
Online Access:https://doi.org/10.1029/2023SW003664
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author Kirolosse M. Girgis
Tohru Hada
Akimasa Yoshikawa
Shuichi Matsukiyo
Viviane Pierrard
Susan W. Samwel
author_facet Kirolosse M. Girgis
Tohru Hada
Akimasa Yoshikawa
Shuichi Matsukiyo
Viviane Pierrard
Susan W. Samwel
author_sort Kirolosse M. Girgis
collection DOAJ
description Abstract During a few solar energetic particle (SEP) events, solar protons were trapped within the geomagnetic field and reached the outer edge of the inner radiation belt. We reproduced this phenomenon by modeling the proton flux distribution at the Low‐Earth Orbit (LEO) for different geomagnetic conditions during solar particle events. We developed a three‐dimensional relativistic test particle simulation code to compute the 70–180 MeV solar proton Lorentz trajectories in low L‐shell range from 1 to 3. The Tsyganenko model (T01) generated the background static magnetic field with the IGRF (v12) model. We have selected three Dst index values: −7, −150, and −210 nT, to define quiet time, strong, and severe geomagnetic storms and to generate the corresponding inner magnetic field configurations. Our results showed that the simulated solar proton flux was more enhanced in the high‐latitude regions and more expanded toward the lower latitude range as long as the geomagnetic storm was intensified. Satellite observations and geomagnetic cutoff rigidities confirmed the numerical results. Furthermore, the LEO proton flux distribution was deformed, so the structure of the proton flux inside the South Atlantic Anomaly (SAA) became longitudinally extended as the Dst index decreased. Moreover, we have assessed the corresponding radiation environment of the LEO mission. We realized that, for a higher inclined LEO mission during an intense geomagnetic storm (Dst = −210 nT), the probability of the occurrence of the Single Event Upset (SEU) rates increased by 19% and the estimated accumulated absorbed radiation doses increased by 17% in comparison with quiet conditions.
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institution Kabale University
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spelling doaj-art-33848f20f1a74accbd0f1effea0f81532025-01-14T16:30:45ZengWileySpace Weather1542-73902023-12-012112n/an/a10.1029/2023SW003664Geomagnetic Storm Effects on the LEO Proton Flux During Solar Energetic Particle EventsKirolosse M. Girgis0Tohru Hada1Akimasa Yoshikawa2Shuichi Matsukiyo3Viviane Pierrard4Susan W. Samwel5International Research Center for Space and Planetary Environmental Science (i‐SPES) Kyushu University Fukuoka JapanInternational Research Center for Space and Planetary Environmental Science (i‐SPES) Kyushu University Fukuoka JapanInternational Research Center for Space and Planetary Environmental Science (i‐SPES) Kyushu University Fukuoka JapanInternational Research Center for Space and Planetary Environmental Science (i‐SPES) Kyushu University Fukuoka JapanRoyal Belgian Institute for Space Aeronomy Solar‐Terrestrial Centre of Excellence Brussels BelgiumNational Research Institute of Astronomy and Geophysics (NRIAG) Helwan EgyptAbstract During a few solar energetic particle (SEP) events, solar protons were trapped within the geomagnetic field and reached the outer edge of the inner radiation belt. We reproduced this phenomenon by modeling the proton flux distribution at the Low‐Earth Orbit (LEO) for different geomagnetic conditions during solar particle events. We developed a three‐dimensional relativistic test particle simulation code to compute the 70–180 MeV solar proton Lorentz trajectories in low L‐shell range from 1 to 3. The Tsyganenko model (T01) generated the background static magnetic field with the IGRF (v12) model. We have selected three Dst index values: −7, −150, and −210 nT, to define quiet time, strong, and severe geomagnetic storms and to generate the corresponding inner magnetic field configurations. Our results showed that the simulated solar proton flux was more enhanced in the high‐latitude regions and more expanded toward the lower latitude range as long as the geomagnetic storm was intensified. Satellite observations and geomagnetic cutoff rigidities confirmed the numerical results. Furthermore, the LEO proton flux distribution was deformed, so the structure of the proton flux inside the South Atlantic Anomaly (SAA) became longitudinally extended as the Dst index decreased. Moreover, we have assessed the corresponding radiation environment of the LEO mission. We realized that, for a higher inclined LEO mission during an intense geomagnetic storm (Dst = −210 nT), the probability of the occurrence of the Single Event Upset (SEU) rates increased by 19% and the estimated accumulated absorbed radiation doses increased by 17% in comparison with quiet conditions.https://doi.org/10.1029/2023SW003664
spellingShingle Kirolosse M. Girgis
Tohru Hada
Akimasa Yoshikawa
Shuichi Matsukiyo
Viviane Pierrard
Susan W. Samwel
Geomagnetic Storm Effects on the LEO Proton Flux During Solar Energetic Particle Events
Space Weather
title Geomagnetic Storm Effects on the LEO Proton Flux During Solar Energetic Particle Events
title_full Geomagnetic Storm Effects on the LEO Proton Flux During Solar Energetic Particle Events
title_fullStr Geomagnetic Storm Effects on the LEO Proton Flux During Solar Energetic Particle Events
title_full_unstemmed Geomagnetic Storm Effects on the LEO Proton Flux During Solar Energetic Particle Events
title_short Geomagnetic Storm Effects on the LEO Proton Flux During Solar Energetic Particle Events
title_sort geomagnetic storm effects on the leo proton flux during solar energetic particle events
url https://doi.org/10.1029/2023SW003664
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AT akimasayoshikawa geomagneticstormeffectsontheleoprotonfluxduringsolarenergeticparticleevents
AT shuichimatsukiyo geomagneticstormeffectsontheleoprotonfluxduringsolarenergeticparticleevents
AT vivianepierrard geomagneticstormeffectsontheleoprotonfluxduringsolarenergeticparticleevents
AT susanwsamwel geomagneticstormeffectsontheleoprotonfluxduringsolarenergeticparticleevents