4.3 Article

Cross-comparison of global simulation models applied to Mercury's dayside magnetosphere

期刊

PLANETARY AND SPACE SCIENCE
卷 198, 期 -, 页码 -

出版社

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.pss.2021.105176

关键词

Mercury; BepiColombo; Modeling

资金

  1. French space plasma physics data center (Center de Donnees de la Physique des Plasmas, CDPP - CNES)
  2. French space plasma physics data center (Center de Donnees de la Physique des Plasmas, CDPP - CNRS)
  3. NASA's Solar System Exploration Research Virtual Institute (SSERVI): Institute for Modeling Plasmas, Atmosphere, and Cosmic Dust (IMPACT)
  4. NASA High-End Computing (HEC) Program through the NASA Advanced Supercomputing (NAS) Division at Ames Research Center
  5. German Ministerium fur Wirtschaft und Energie
  6. German Zentrum fur Luft-und Raumfahrt [50 QW 1501]
  7. DFG (German Research Foundation) [HE8016/1-1]
  8. Swedish National Research Council [2018-03454]
  9. Swedish National Space Agency [2018-C, 2018-N]
  10. Swedish National Infrastructure for Computing (SNIC) at the High Performance Computing Center North (HPC2N), Umea University, Sweden [SNIC2019/3-178, SNIC2020-5-101]
  11. CNES
  12. European Union's Horizon 2020 research and innovation programme [871149]
  13. Vinnova [2018-03454] Funding Source: Vinnova
  14. Swedish Research Council [2018-03454] Funding Source: Swedish Research Council

向作者/读者索取更多资源

This study compares the results of multiple global simulations of the interaction between the solar wind and Mercury, providing accurate predictions of the structure of Mercury's magnetosphere and aiding in the analysis of onboard plasma measurements from past and future missions to Mercury.
We present the first comparison of multiple global simulations of the solar wind interaction with Mercury's dayside magnetosphere, conducted in the framework of the international collaborative project SHOTS - Studies on Hermean magnetosphere Oriented Theories and Simulations. Two 3D magnetohydrodynamic and two 3D hybrid simulation codes are used to investigate the global response of the Hermean magnetosphere without its exosphere to a northward-oriented interplanetary magnetic field. We cross-compare the results of the four codes for a theoretical case and a MESSENGER orbit with similar upstream plasma conditions. The models agree on bowshock and magnetopause locations at 2.1 +/- 0.11 and 1.4 +/- 0.1 Mercury planetary radii, respectively. The latter locations may be influenced by subtle differences in the treatment of the plasma boundary at the planetary surface. The predicted magnetosheath thickness varies less between the codes. Finally, we also sample the plasma data along virtual trajectories of BepiColombo's Magnetospheric and Planetary Orbiter. Our ability to accurately predict the structure of the Hermean magnetosphere aids the analysis of the onboard plasma measurements of past and future magnetospheric missions.

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