Wave-Number Spectra and Intermittency in the Terrestrial Foreshock Region

Y. Narita, K.-H. Glassmeier, and R. A. Treumann
Phys. Rev. Lett. 97, 191101 – Published 8 November 2006

Abstract

Wave-number spectra of magnetic field fluctuations are directly determined in the terrestrial foreshock region (upstream of a quasiparallel collisionless shock wave) using four-point Cluster spacecraft measurements. The spectral curve is characterized by three ranges reminiscent of turbulence: energy injection, inertial, and dissipation range. The spectral index for the inertial range spectrum is close to Kolmogorov’s slope, 5/3. On the other hand, the fluctuations are highly anisotropic and intermittent perpendicular to the mean magnetic field direction. These results suggest that the foreshock is in a weakly turbulent and intermittent state in which parallel propagating Alfvén waves interact with one another, resulting in the phase coherence or the intermittency.

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  • Received 14 November 2005

DOI:https://doi.org/10.1103/PhysRevLett.97.191101

©2006 American Physical Society

Authors & Affiliations

Y. Narita* and K.-H. Glassmeier

  • Institute of Geophysics and Extraterrestrial Physics, Mendelssohnstrasse 3, D-38106 Braunschweig, Germany

R. A. Treumann

  • Department of Geoscience, Geophysics Section, Ludwig-Maximilians-University Munich, Theresienstrasse 41, D-80333 Munich, Germany

  • *Electronic address: y.narita@tu-bs.de
  • Also at Max Planck Institute for Solar System Research, Katlenburg-Lindau, Germany.
  • Senior visiting scientist at International Space Science Institute, Berne, Switzerland.

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Issue

Vol. 97, Iss. 19 — 10 November 2006

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