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On the Spatial Relationship Between the Aurora and Relativistic Electron Precipitation During a Storm‐Time Substorm
Journal article   Open access   Peer reviewed

On the Spatial Relationship Between the Aurora and Relativistic Electron Precipitation During a Storm‐Time Substorm

M Shumko, A. Artemyev, S. Raptis, Y. Zou, D. L. Turner, A. Y. Ukhorskiy, C. Gabrielse, G. K. Stephens, I. J. Cohen, C. Wilkins, …
Geophysical research letters, Vol.52(17), e2025GL116477
09/16/2025
DOI: 10.1029/2025GL116477
url
https://doi.org/10.1029/2025GL116477View
Published (Version of record) Open Access

Abstract

During substorms, Earth's magnetotail undergoes rapid dipolarization, driving Earthward plasma flows that decelerate and dissipate energy upon encountering the dipole magnetic field in the nightside transition region. This region mediates the interaction between the magnetotail, inner magnetosphere, and the ionospheric auroral zone, though significant mapping uncertainties obscure the precise link and particle acceleration processes. Using data from THEMIS, TREx, and ELFIN, we analyze a storm‐time substorm on 4 September 2022, establishing a relationship, that is, not a causation, between magnetospheric and ionospheric dynamics. Following a dipolarization, the auroral bulge overlapped with the footprints of the electron isotropy boundary (IB) and the outer radiation belt. Notably, the precipitating electron energies reached at least 2 MeV in the bulge, exceeding previous reports. By comparing the latitudes of the electron IB with respect to the auroral bulge, we deduce that the sources of both auroral and relativistic precipitation were confined in the dipolarized region. Plain Language Summary Explosive magnetospheric substorms and beautiful auroral displays are signatures of rapid reconfiguration of Earth's magnetic field from a stretched to a more dipolar configuration. The global reconfiguration is known as dipolarization, a phenomenon that occurs simultaneously with bright auroral displays. The dipolarization, aurora, and the hazardous radiation belt (RB) electrons are likely linked, though significant magnetic mapping uncertainties obscure the precise link and the particle acceleration processes involved. Here, we study this system with a fortuitous combination of satellites and ground‐based auroral imagers. After a dipolarization, the aurora overlapped with the energetic electrons prescribed to the outer RB. These findings reveal that during the peak of a substorm, the bright part of the auroral oval is sometimes contained within the newly reconfigured magnetic field, highlighting the intricate relationship between cislunar space and Earth's atmosphere. Key Points During a storm‐time substorm, 2 MeV electron precipitation was associated with the auroral bulge The magnetospheric source region of the auroral bulge and the radiation belt (RB) overlapped during this substorm We deduce that the source region of the auroral bulge and RB electrons was in the newly dipolarized magnetosphere
dipolarization ELFIN isotropy boundary radiation belt substorm THEMIS TREx

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