Issue |
A&A
Volume 681, January 2024
|
|
---|---|---|
Article Number | A98 | |
Number of page(s) | 6 | |
Section | Planets and planetary systems | |
DOI | https://doi.org/10.1051/0004-6361/202347789 | |
Published online | 23 January 2024 |
Solar wind entry into Mercury’s magnetosphere: Simulation results for the second swingby of BepiColombo
1
Space Research Institute Graz, Austrian Academy of Sciences,
Graz,
Austria
e-mail: daniel.teubenbacher@oeaw.ac.at
2
Institute of Physics/IGAM, University of Graz,
Graz,
Austria
3
European Space Agency, ESTEC,
Noordwijk,
The Netherlands
4
Institut für Theoretische Physik, Technische Universität Braunschweig,
Braunschweig,
Germany
5
Institut für Geophysik und Extraterrestrische Physik, Technische Universität Braunschweig,
Braunschweig,
Germany
6
Institute for Space Science, National Institute for Laser, Plasma and Radiation Physics,
Măgurele,
Romania
Received:
23
August
2023
Accepted:
16
November
2023
Context. We use a global 3D hybrid plasma model to investigate the interaction between Mercury’s magnetosphere and the solar wind for the second BepiColombo swingby, evaluate magnetospheric regions, and study the typical energy profile of protons.
Aims. The objective of this study is to gain a better understanding of solar wind entry and analyze simulated plasma data along a trajectory using BepiColombo swingby 2 conditions, with the goal of enhancing our comprehension of measurement data and potentially providing forecasts for future swingbys.
Methods. To model Mercury’s plasma environment, we used the hybrid code AIKEF and developed a method to extract the particle (ion) data in order to compute the proton energy spectrum along the trajectory of BepiColombo during its second Mercury swingby on June 23, 2022. We evaluate magnetopause and bow shock stand-off distances under average upstream solar wind conditions with the Interplanetary Magnetic Field (IMF) condition derived from the BepiColombo magnetic field measurements during the second Mercury swingby.
Results. We found that the magnetosheath on the quasi-perpendicular (dusk) side of the bow shock is thicker than that on the quasi-parallel (dawn) side, where a foreshock is formed. Multiple plasma populations can be extracted from our modeled energy spectra that assist in identifying magnetospheric regions. We observed protons of solar wind origin entering Mercury’s magnetosphere. Their energies range from a few electron volts in the magnetosphere up to 10 keV in the magnetosheath.
Key words: plasmas / methods: numerical / planets and satellites: terrestrial planets / planet-star interactions
© The Authors 2024
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.
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