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Direct Measurement of Low‐Energy Electron Foreshock Beams

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    0510734 - ÚFA 2020 RIV US eng J - Journal Article
    Souček, Jan - Píša, David - Santolík, Ondřej
    Direct Measurement of Low‐Energy Electron Foreshock Beams.
    Journal of Geophysical Research-Space Physics. Roč. 124, č. 4 (2019), s. 2380-2392. ISSN 2169-9380. E-ISSN 2169-9402
    R&D Projects: GA ČR(CZ) GA17-08772S; GA ČR(CZ) GJ16-16050Y
    Grant - others:AV ČR(CZ) AP1401
    Program: Akademická prémie - Praemium Academiae
    Institutional support: RVO:68378289
    Keywords : plasma waves upstream * high-frequency waves * ion-sound-waves * Langmuir-waves * solar-wind * nonthermal electrons * decay * oscillations * mode
    OECD category: Fluids and plasma physics (including surface physics)
    Impact factor: 2.799, year: 2019
    Method of publishing: Limited access
    https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2019JA026470

    Electrostatic plasma waves above and below the local electron plasma frequency represent a characteristic feature of the foreshock region. These waves are known to be generated by electron beams originating from the bow shock and their spectrum varies from narrowband intense waves close to foreshock edge to weaker broadband emissions further downstream. We present a statistical analysis of electron beams observed in the terrestrial foreshock by the Cluster spacecraft. We compared the energy of foreshock electron beams with the spectrum of electrostatic waves and established a clear correspondence between beam energy and spectrum of the waves. The broadband emissions are correlated with low-energy beams, while high-energy electron beams are associated with narrowband Langmuir waves. Next we solved the linear dispersion relation for a subset of observed electron plasma distributions. We discovered that while the observed electron distributions often exhibit a 'bump on tail' feature necessary for an instability, the observed combination of beam energy, density, and temperature typically corresponds to a stable situation. This indicates that strongly unstable electron beams are quickly dissipated by the quasi-linear processes and only stable or marginally stable beams persist long enough to be observed by the instrument.
    Permanent Link: http://hdl.handle.net/11104/0301137

     
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