Published April 2025 | Published
Journal Article Open

Investigation of the inverse velocity dispersion in a solar energetic particle event observed by Solar Orbiter

  • 1. ROR icon Kiel University
  • 2. Johns Hopkins Applied Physics Lab, Laurel, MD, 20723, USA
  • 3. ROR icon KU Leuven
  • 4. ROR icon University of Science and Technology of China
  • 5. ROR icon University of Graz
  • 6. ROR icon University of Alcalá
  • 7. ROR icon Southwest Research Institute
  • 8. ROR icon California Institute of Technology

Abstract

Context. Solar energetic particle (SEP) events provide crucial insights into particle acceleration and transport mechanisms in the heliosphere. Inverse velocity dispersion (IVD) events, characterized by higher-energy particles that arrive later than lower-energy particles, challenge the classical understanding of SEP events and are increasingly observed by spacecraft, such as Parker Solar Probe and Solar Orbiter. However, the mechanisms underlying IVD events remain poorly understood.

Aims. We investigate the physical processes that cause long-duration IVD events by analyzing the SEP event observed by Solar Orbiter on 2022 June 7. We explore the role of evolving shock connectivity, particle acceleration at interplanetary (IP) shocks, and cross-field transport in shaping the observed particle profiles.

Methods. We used data from the Energetic Particle Detector (EPD) suite on board Solar Orbiter to analyze the characteristics of the IVD, and we modeled the event using the heliospheric energetic particle acceleration and transport (HEPAT) model. The simulations tracked evolutions of shock properties, particle acceleration and transport to assess the influence of shock expansion, shock connectivity, and transport processes on the formation of IVD events.

Results. The IVD event exhibited a distinct and long-duration IVD signature across proton energies from 1 to 20 MeV, and it lasted for approximately 10 hours. Heavy ions exhibited varying nose energies, defined as the energy corresponding to the first-arriving particles. Simulations suggest that evolving shock connectivity and the evolution of the shock play a primary role in the IVD signature. The magnetic connection shifts from the shock flank to the nose over time, which results in a gradual increase in the maximum particle energy along the field line. Furthermore, the model results show that limited cross-field diffusion can influence both the nose energy and the duration of the IVD event.

Conclusions. This study demonstrates that long-duration IVD events are primarily driven by evolving magnetic connectivity along a nonuniform shock that evolves over time, where the connection moves to more efficient acceleration sites as the shock propagates farther from the Sun. Other mechanisms, such as the acceleration time at the shock, may also contribute to the observed IVD features. The interplay of these factors remains an open question that warrants further investigation in other events.

Copyright and License

© The Authors 2025. Open Access article, published by EDP Sciences, under the terms of the Creative Commons Attribution License (https://creativecommons.org/licenses/by/4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

Acknowledgement

We thank Gary Zank for his helpful comments. Solar Orbiter is a mission of international cooperation between ESA and NASA, operated by ESA. This work was supported by the German Federal Ministry for Economic Affairs and Energy and the German Space Agency (Deutsches Zentrum für Luft- und Raumfahrt, e.V., (DLR)), grant number 50OT2002. The UAH team acknowledges the financial support by Project PID2023-150952OB-I00 funded by MICIU/AEI/10.13039/501100011033 and by FEDER, UE. The Suprathermal Ion Spectrograph (SIS) is a European facility instrument funded by ESA under contract number SOL.ASTR.CON.00004. Solar Orbiter post-launch work at JHU/APL and the Southwest Research Institute is supported by NASA contract NNN06AA01C. This research was supported in part through high-performance computing resources available at the Kiel University Computing Centre.

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Additional details

Created:
April 22, 2025
Modified:
April 22, 2025