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    Electron Bulk Acceleration and Thermalization at Earth’s Quasiperpendicular Bow Shock

    L.-J. Chen1,2,*, S. Wang1,2, L. B. Wilson, III1, S. Schwartz3, N. Bessho1,2, T. Moore1, D. Gershman1, B. Giles1, D. Malaspina3 et al.

    F. D. Wilder3, R. E. Ergun3, M. Hesse4, H. Lai5, C. Russell5, R. Strangeway5, R. B. Torbert6, A. F.-Vinas1, J. Burch6, S. Lee1, C. Pollock7, J. Dorelli1, W. Paterson1, N. Ahmadi3, K. Goodrich3, B. Lavraud8, O. Le Contel9, Yu. V. Khotyaintsev10, P.-A. Lindqvist11, S. Boardsen1,2, H. Wei5, A. Le12, and L. Avanov1,2

    • 1NASA, Goddard Space Flight Center, Greenbelt, Maryland 20771, USA
    • 2Department of Astronomy, University of Maryland, College Park, Maryland 20747, USA
    • 3Laboratory for Atmospheric and Space Physics, University of Colorado, Boulder, Colorado 80305, USA
    • 4University of Bergen, Bergen 5020, Norway
    • 5University of California, Los Angeles, Los Angeles, California 90095, USA
    • 6Southwest Research Institute, San Antonio, Texas 78238, USA
    • 7Denali Scientific, Healy, Alaska 99743, USA
    • 8Institut de Recherche en Astrophysique et Planétologie, Université de Toulouse (UPS), CNRS, CNES, Toulouse, 31028 Cedex 4, France
    • 9Laboratoire de Physique des Plasmas (UMR7648), CNRS/Ecole Polytechnique/Sorbonne Université/Univ. Paris Sud/Observatoire de Paris, Paris, F91128 Palaiseau Cedex, France
    • 10Swedish Institute of Space Physics, Uppsala SE-75121, Sweden
    • 11KTH Royal Institute of Technology, Stockholm SE-11428, Sweden
    • 12Los Alamos National Laboratory, Los Alamos, New Mexico 87545, USA

    • *lijen@mailaps.org

    Phys. Rev. Lett. 120, 225101 – Published 31 May, 2018

    DOI: https://doi.org/10.1103/PhysRevLett.120.225101

    Abstract

    Electron heating at Earth’s quasiperpendicular bow shock has been surmised to be due to the combined effects of a quasistatic electric potential and scattering through wave-particle interaction. Here we report the observation of electron distribution functions indicating a new electron heating process occurring at the leading edge of the shock front. Incident solar wind electrons are accelerated parallel to the magnetic field toward downstream, reaching an electron-ion relative drift speed exceeding the electron thermal speed. The bulk acceleration is associated with an electric field pulse embedded in a whistler-mode wave. The high electron-ion relative drift is relaxed primarily through a nonlinear current-driven instability. The relaxed distributions contain a beam traveling toward the shock as a remnant of the accelerated electrons. Similar distribution functions prevail throughout the shock transition layer, suggesting that the observed acceleration and thermalization is essential to the cross-shock electron heating.

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