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Hybrid modeling of cometary plasma environments: II. Remote-sensing of a cometary bow shock

  • University of Michigan, Ann Arbor
  • University of Oslo
  • Swedish Institute of Space Physics
  • Luleå University of Technology
  • Finnish Meteorological Institute

Research output: Contribution to journalArticleScientificpeer-review

18 Citations (Scopus)
207 Downloads (Pure)

Abstract

Context. The ESA Rosetta probe has not seen direct evidence of a fully formed bow shock at comet 67P/Churyumov-Gerasimenko (67P). Ion spectrometer measurements of cometary pickup ions measured in the vicinity of the nucleus of 67P are available and may contain signatures of the large-scale plasma environment. Aims. The aim is to investigate the possibility of using pickup ion signatures to infer the existence or nonexistence of a bow shock-like structure and possibly other large-scale plasma environment features. Methods. A numerical plasma model in the hybrid plasma description was used to model the plasma environment of a comet. Simulated pickup ion spectra were generated for different interplanetary magnetic field conditions. The results were interpreted through test particle tracing in the hybrid simulation solutions. Results. Features of the observed pickup ion energy spectrum were reproduced, and the model was used to interpret the observation to be consistent with a shock-like structure. We identify (1) a spectral break related to the bow shock, (2) a mechanism for generating the spectral break, and (3) a dependency of the energy of the spectral break on the interplanetary magnetic field magnitude and bow shock standoff distance.

Original languageEnglish
Article numberA45
Number of pages16
JournalAstronomy & Astrophysics
Volume630
Early online date27 Feb 2019
DOIs
Publication statusPublished - 1 Oct 2019
MoE publication typeA1 Journal article-refereed

Funding

M.A. acknowledges financial support from the Aino and Kaarlo Tiisala Foundation and the RPC meetings for fruitful discussions. C.S.W. was funded at University of Oslo by the Norwegian Research Council ?Rosetta? grant no. 240000. The authors acknowledge ISSI (Bern) and the ISSI International Team ?Plasma Environment of comet 67P after Rosetta? for fruitful discussions and collaborations. Aalto Science-IT is recognized for providing computational capacities. The Lawrence Livermore National Laboratories visualization software VisIt was used for the analysis of the simulations and the production of some publication figures. The authors would also like to thank R. Munroe (xkcd) for inspiring us in the use of sophisticated curve-smoothing technique

Keywords

  • Comets: general
  • Comets: individual: 67P/Churyumov-Gerasimenko
  • Methods: numerical
  • Plasmas
  • Shock waves
  • Techniques: miscellaneous

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