Observations of Slow Electron Holes at a Magnetic Reconnection Site

Yu. V. Khotyaintsev, A. Vaivads, M. André, M. Fujimoto, A. Retinò, and C. J. Owen
Phys. Rev. Lett. 105, 165002 – Published 12 October 2010

Abstract

We report in situ observations of high-frequency electrostatic waves in the vicinity of a reconnection site in the Earth’s magnetotail. Two different types of waves are observed inside an ion-scale magnetic flux rope embedded in a reconnecting current sheet. Electron holes (weak double layers) produced by the Buneman instability are observed in the density minimum in the center of the flux rope. Higher frequency broadband electrostatic waves with frequencies extending up to fpe are driven by the electron beam and are observed in the denser part of the rope. Our observations demonstrate multiscale coupling during the reconnection: Electron-scale physics is induced by the dynamics of an ion-scale flux rope embedded in a yet larger-scale magnetic reconnection process.

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  • Received 9 July 2010

DOI:https://doi.org/10.1103/PhysRevLett.105.165002

© 2010 The American Physical Society

Authors & Affiliations

Yu. V. Khotyaintsev*, A. Vaivads, and M. André

  • Swedish Institute of Space Physics, Uppsala, Sweden

M. Fujimoto

  • Institute of Space and Astronautical Science, Japan Aerospace Exploration Agency, Sagamihara, Japan

A. Retinò

  • Space Research Institute, Austrian Academy of Sciences, Graz, Austria

C. J. Owen

  • Mullard Space Science Laboratory, University College London, Dorking, United Kingdom

  • *yuri@irfu.se

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Issue

Vol. 105, Iss. 16 — 15 October 2010

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