Abstract
The auroral acceleration region plays an important role in the magnetosphere-ionosphere coupling system. In this study, signatures of an auroral U-shaped potential structure were found for the first time in the near-equatorial inner magnetosphere by the Arase satellite at ∼6.0 RE geocentric distance and 11° magnetic latitude. The observed magnetic and electric field variations corresponded to the equatorward motion of the upward field-aligned current and converging perpendicular electric field. Examining the three-dimensional velocity distribution function of H+ and O+ ions, we demonstrate that upflowing ion beams were significantly deflected in an east-west direction with a perpendicular velocity up to ∼80 km/s, which is consistent with the ExB drift velocity. A simple particle drift model with the inferred auroral perpendicular potential presents a new kink-like drift path of ions from the magnetotail, implying that the auroral potential structure has a great impact on particle dynamics in the near-earth plasma sheet.
Original language | English |
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Article number | e2022GL098105 |
Journal | Geophysical Research Letters |
Volume | 49 |
Issue number | 10 |
DOIs | |
Publication status | Published - 2022 May 28 |
Keywords
- auroral acceleration region
- inner magnetosphere
- plasma convection
- upflowing ion beam
ASJC Scopus subject areas
- Geophysics
- Earth and Planetary Sciences(all)