Publications

2024

Mercury's plasma environment after BepiColombo's third flyby
- Hadid Lina Z.
- Delcourt Dominique
- Harada Yuki
- Rojo Mathias
- Aizawa Sae
- Saito Yoshifumi
- André Nicolas
- Glass Austin N.
- Raines Jim M.
- Yokota Shoichiro
- Fränz Markus
- Katra Bruno
- Verdeil Christophe
- Fiethe Björn
- Leblanc François
- Modolo Ronan
- Fontaine Dominique
- Krupp Norbert
- Krüger Harald
- Leblanc Frédéric
- Fischer Henning
- Berthelier Jean-Jacques
- Sauvaud Jean-André
- Murakami Go
- Matsuda Shoya
Communications Physics, Nature Research, 2024, 7, pp.316. 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. (10.1038/s42005-024-01766-8)
DOI : 10.1038/s42005-024-01766-8
Structure and dynamics of the Hermean magnetosphere revealed by electron observations from the Mercury electron analyzer after the first three Mercury flybys of BepiColombo
- Rojo M.
- André N.
- Aizawa S.
- Sauvaud J.-A.
- Saito Y.
- Harada Y.
- Fedorov A.
- Penou E.
- Barthe A.
- Persson M.
- Yokota S.
- Mazelle C.
- Hadid L. Z.
- Delcourt D.
- Fontaine D.
- Fränz M.
- Katra B.
- Krupp N.
- Murakami G.
Astronomy & Astrophysics - A&A, EDP Sciences, 2024, 687, pp.A243. Context. The Mercury electron analyzer (MEA) obtained new electron observations during the first three Mercury flybys by BepiColombo on October 1, 2021 (MFB1), June 23 , 2022 (MFB2), and June 19, 2023 (MFB3). BepiColombo entered the dusk side magnetotail from the flank magnetosheath in the northern hemisphere, crossed the Mercury solar orbital equator around midnight in the magnetotail, traveled from midnight to dawn in the southern hemisphere near the closest approach, and exited from the post-dawn magnetosphere into the dayside magnetosheath.Aims. We aim to identify the magnetospheric boundaries and describe the structure and dynamics of the electron populations observed in the various regions explored along the flyby trajectories.Methods. We derive 4s time resolution electron densities and temperatures from MEA observations. We compare and contrast our new BepiColombo electron observations with those obtained from the Mariner 10 scanning electron spectrometer (SES) 49 yr ago.Results. A comparison to the averaged magnetospheric boundary crossings of MESSENGER indicates that the magnetosphere of Mercury was compressed during MFB1, close to its average state during MFB2, and highly compressed during MFB3. Our new MEA observations reveal the presence of a wake effect very close behind Mercury when BepiColombo entered the shadow region, a significant dusk-dawn asymmetry in electron fluxes in the nightside magnetosphere, and strongly fluctuating electrons with energies above 100s eV in the dawnside magnetosphere. Magnetospheric electron densities and temperatures are in the range of 10–30 cm−3 and above a few 100s eV in the pre-midnight-sector, and in the range of 1–100 cm−3 and well below 100 eV in the post-midnight sector, respectively.Conclusions. The MEA electron observations of different solar wind properties encountered during the first three Mercury flybys reveal the highly dynamic response and variability of the solar wind-magnetosphere interactions at Mercury. A good match is found between the electron plasma parameters derived by MEA in the various regions of the Hermean environment and similar ones derived in a few cases from other instruments on board BepiColombo. (10.1051/0004-6361/202449450)
DOI : 10.1051/0004-6361/202449450
Extent of the Magnetotail of Venus From the Solar Orbiter, Parker Solar Probe and BepiColombo Flybys
- Edberg Niklas
- Andrews David
- Boldú J. Jordi
- Dimmock Andrew
- Khotyaintsev Yuri
- Kim Konstantin
- Persson Moa
- Auster Uli
- Constantinescu Dragos
- Heyner Daniel
- Mieth Johannes
- Richter Ingo
- Curry Shannon
- Hadid Lina
- Pisa David
- Sorriso-Valvo Luca
- Lester Mark
- Sánchez-Cano Beatriz
- Stergiopoulou Katerina
- Romanelli Norberto
- Fischer David
- Schmid Daniel
- Volwerk Martin
Journal of Geophysical Research Space Physics, American Geophysical Union/Wiley, 2024, 129 (10), pp.e2024JA032603. We analyze data from multiple flybys by the Solar Orbiter, BepiColombo, and Parker Solar Probe (PSP) missions to study the interaction between Venus' plasma environment and the solar wind forming the induced magnetosphere. Through examination of magnetic field and plasma density signatures we characterize the spatial extent and dynamics of Venus' magnetotail, focusing mainly on boundary crossings. Notably, we observe significant differences in boundary crossing location and appearance between flybys, highlighting the dynamic nature of Venus' magnetotail. In particular, during Solar Orbiter's third flyby, extreme solar wind conditions led to significant variations in the magnetosheath plasma density and magnetic field properties, but the increased dynamic pressure did not compress the magnetotail. Instead, it is possible that the increased EUV flux at this time rather caused it to expand in size. Key findings also include the identification of several far downstream bow shock (BS), or bow wave, crossings to at least 60 (1 = 6,052 km is the radius of Venus), and the induced magnetospheric boundary to at least 20 . These crossings provide insight into the extent of the induced magnetosphere. Pre‐existing models from Venus Express were only constrained to within 5 of the planet, and we provide modifications to better fit the far‐downstream crossings. The new model BS is now significantly closer to the central tail than previously suggested, by about 10 at 60 downstream. (10.1029/2024JA032603)
DOI : 10.1029/2024JA032603

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