Anisotropy of Solar Wind Turbulence between Ion and Electron Scales

C. H. K. Chen, T. S. Horbury, A. A. Schekochihin, R. T. Wicks, O. Alexandrova, and J. Mitchell
Phys. Rev. Lett. 104, 255002 – Published 25 June 2010

Abstract

The anisotropy of turbulence in the fast solar wind, between the ion and electron gyroscales, is directly observed using a multispacecraft analysis technique. Second order structure functions are calculated at different angles to the local magnetic field, for magnetic fluctuations both perpendicular and parallel to the mean field. In both components, the structure function value at large angles to the field S is greater than at small angles S: in the perpendicular component S/S=5±1 and in the parallel component S/S>3, implying spatially anisotropic fluctuations, k>k. The spectral index of the perpendicular component is 2.6 at large angles and 3 at small angles, in broad agreement with critically balanced whistler and kinetic Alfvén wave predictions. For the parallel component, however, it is shallower than 1.9, which is considerably less steep than predicted for a kinetic Alfvén wave cascade.

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  • Received 10 February 2010

DOI:https://doi.org/10.1103/PhysRevLett.104.255002

©2010 American Physical Society

Authors & Affiliations

C. H. K. Chen1,*, T. S. Horbury1, A. A. Schekochihin2, R. T. Wicks1, O. Alexandrova3, and J. Mitchell1

  • 1The Blackett Laboratory, Imperial College London, London SW7 2AZ, United Kingdom
  • 2Rudolf Peierls Centre for Theoretical Physics, University of Oxford, Oxford OX1 3NP, United Kingdom
  • 3LESIA, Observatoire de Paris, CNRS, UPMC, Université Paris Diderot, 92190 Meudon, France

  • *christopher.chen03@imperial.ac.uk

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Vol. 104, Iss. 25 — 25 June 2010

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