Abstract
Whistler-mode chorus waves are natural electromagnetic emissions known to play a key role in electron acceleration and loss mechanisms via wave–particle interactions in planetary magnetospheres. Chorus waves have not yet been detected in Mercury’s magnetosphere due to the lack of suitable instruments in the probes that previously visited the planet as well as to its harsh environment. Here, we present the direct probing of chorus waves in the localized dawn sector during the first and second Mercury flybys by the BepiColombo/Mio spacecraft. Mio’s search coil magnetometers detected chorus events with tens of picotesla intensities in the dawn sector, while no clear chorus activity was observed in the night sector. The simulation results suggest that this regional difference could be due to the impact of background magnetic field inhomogeneities on the nonlinear wave generation process. This observational evidence is crucial for understanding the energetic electron dynamics of the localized dawn sector of Mercury’s magnetosphere.
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Data availability
The spacecraft orbit data are available from SPICE data for BepiColombo https://www.cosmos.esa.int/web/spice/spice-for-bepicolombo. The PWI raw data are available from https://doi.org/10.5281/zenodo.8026227 (in a Zenodo repository). The PWI team (Yasumasa Kasaba, principal investigator; kasaba.y@tohoku.ac.jp) and the corresponding author can provide the PWI raw data upon reasonable request. Source data are provided with this paper.
Code availability
The particle-in-cell simulations are based on the literature36,45 and the PIC code (KEMPO1) is available at http://space.rish.kyoto-u.ac.jp/software/.
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Acknowledgements
We express our sincere thanks to all the Mio and BepiColombo project members for their careful contributions to the projects’ operations. We gratefully acknowledge H. Kojima, K. Issautier, J.-E. Wahlund and all the PWI members for their careful support to the PWI operations. The Japanese authors express their deep appreciation to H. Matsumoto, I. Nagano and H. Hayakawa for their valuable comments during the development of the PWI. This study was supported in part by the Japan Society for the Promotion of Science, KAKENHI grant no. JP20H02162 (M.O.) and the Mitani Foundation for Research and Development (M.O.). This paper is based on observations obtained with BepiColombo, a joint European Space Agency (ESA)–Japan Aerospace Exploration Agency (JAXA) science mission with instruments and contributions directly funded by the ESA Member States and JAXA. The French participation in the BepiColombo mission is funded by Centre National d’Etudes Spatiales (F.S., L.M. and G.C.).
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Contributions
M.O. developed the scientific content of this study, analysed the search coil data, numerically computed the chorus waves modelled in Mercury’s environment, wrote this paper, produced the figures and contributed to the development of the low-frequency search coil of the PWI. S.Y. led the development of the low-frequency search coil of the PWI and contributed to the PWI data analysis. Y. Kasaba is the principal investigator of the PWI and led the PWI observations during the flybys. Y. Kasahara and S.M. contributed to the PWI data production and analysis. Y.O. and M.H. contributed to the particle-in-cell simulations and the numerical analysis based on the nonlinear wave growth theory and its interpretation. S.K. is a member of the BepiColombo Young Scientists Study Group and contributed to the PWI data analysis. F.S., L.M. and G.C. contributed to the evaluation of the dual-band search coil data and their interpretation and to the editing of this paper. S.N. led the electromagnetic compatibility assessments of the Mio spacecraft and contributed to the improvement of the PWI data by removing spacecraft noise. G.M. is the project scientist and contributed to the Mercury flyby operations. All the authors provided feedback on this paper.
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Nature Astronomy thanks Allison Jaynes, James Slavin and the other, anonymous, reviewer(s) for their contribution to the peer review of this work.
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Supplementary Information
Supplementary Figs. 1–4 and references.
Supplementary Video 1
Video of the first Mercury flyby orbit and the dynamic spectrum of the wave magnetic field on 1 October 2021. The orbit is drawn in Mercury solar magnetic (MSM) coordinates51. The star symbol shows the location of Mio. The solid lines show the orbit, and each dot shows the satellite location every 5 minutes. The green lines show the observed dawn chorus region. The dotted and dashed curves indicate typical locations of the magnetopause and the bow shock52, respectively. The white line indicates the electron gyrofrequency estimated by an empirical model9. The red moving bar in the spectrum traces the time progress. The colour map image of Mercury is published at https://photojournal.jpl.nasa.gov/catalog/PIA17386. Credit: Colour map of Mercury, NASA/Johns Hopkins University Applied Physics Laboratory/Carnegie Institution of Washington.
Supplementary Video 2
Video of the second Mercury flyby orbit and the dynamic spectrum of the wave magnetic field on 23 June 2022. The format is the same as for Supplementary Video 1. The colour map image of Mercury is published at https://photojournal.jpl.nasa.gov/catalog/PIA17386. Credit: colour map of Mercury, NASA/Johns Hopkins University Applied Physics Laboratory/Carnegie Institution of Washington.
Supplementary Data
Source data for Supplementary Videos 1 and 2 and Fig. 1.
Supplementary Data
Source data for Supplementary Fig. 2.
Supplementary Data
Source data for Supplementary Fig. 3.
Supplementary Data
Source data for Supplementary Fig. 4.
Source data
Source Data Fig. 1
Wave magnetic field spectra of whistler-mode waves in Mercury flybys.
Source Data Fig. 2
Observed whistler-mode wave intensity.
Source Data Fig. 3
PIC simulations in Mercury’s environment.
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Ozaki, M., Yagitani, S., Kasaba, Y. et al. Whistler-mode waves in Mercury’s magnetosphere observed by BepiColombo/Mio. Nat Astron 7, 1309–1316 (2023). https://doi.org/10.1038/s41550-023-02055-0
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DOI: https://doi.org/10.1038/s41550-023-02055-0