Communications Physics (Oct 2024)

Mercury’s plasma environment after BepiColombo’s third flyby

  • Lina Z. Hadid,
  • Dominique Delcourt,
  • Yuki Harada,
  • Mathias Rojo,
  • Sae Aizawa,
  • Yoshifumi Saito,
  • Nicolas André,
  • Austin N. Glass,
  • Jim M. Raines,
  • Shoichiro Yokota,
  • Markus Fränz,
  • Bruno Katra,
  • Christophe Verdeil,
  • Björn Fiethe,
  • Francois Leblanc,
  • Ronan Modolo,
  • Dominique Fontaine,
  • Norbert Krupp,
  • Harald Krüger,
  • Frédéric Leblanc,
  • Henning Fischer,
  • Jean-Jacques Berthelier,
  • Jean-André Sauvaud,
  • Go Murakami,
  • Shoya Matsuda

DOI
https://doi.org/10.1038/s42005-024-01766-8
Journal volume & issue
Vol. 7, no. 1
pp. 1 – 7

Abstract

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Abstract Understanding Mercury’s magnetosphere is crucial for advancing our comprehension of how the solar wind interacts with the planetary magnetospheres. Despite previous missions, several gaps remain in our knowledge of Mercury’s plasma environment. Here, we present findings from BepiColombo’s third flyby, offering a synoptic view of the large scale structure and composition of Mercury’s magnetosphere. The Mass Spectrum Analyzer (MSA), Mass Ion Analyzer (MIA), and Mass Electron Analyzer (MEA) on the magnetospheric orbiter reveal insights, including the identification of trapped energetic hydrogen (H+) with energies around 20 keV e−1 evidencing a ring current, and a cold ion plasma with energies below 50 eV e−1. Additionally, we observe a Low-Latitude Boundary Layer (LLBL), which is a region of turbulent plasma at the edge of the magnetosphere, characterized by bursty ion enhancements, indicating an ongoing injection process in the duskside magnetosphere flank. These observations during cruise phase provide a tantalizing glimpse of future discoveries expected from the Mercury Plasma Particle Experiment (MPPE) instruments after orbit insertion, promising broader impacts on our understanding of planetary magnetospheres.