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Title: Wavenumber spectrum of whistler turbulence: Particle-in-cell simulation

Journal Article · · Physics of Plasmas
DOI:https://doi.org/10.1063/1.3526602· OSTI ID:21532084
 [1];  [2];  [3]
  1. Solar-Terrestrial Environment Laboratory, Nagoya University, Nagoya 464-8601 (Japan)
  2. Los Alamos National Laboratory, Los Alamos, New Mexico 87545 (United States)
  3. Institut fuer Geophysik und extraterrestrische Physik, Technische Universitaet Braunschweig, Mendelssohnstr. 3, D-38106 Braunschweig (Germany)

The forward cascade of decaying whistler turbulence is studied in low beta plasma to understand essential properties of the energy spectrum at electron scales, by using a two-dimensional electromagnetic particle-in-cell (PIC) simulation. This simulation demonstrates turbulence in which the energy cascade rate is greater than the dissipation rate at the electron inertial length. The PIC simulation shows that the magnetic energy spectrum of forward-cascaded whistler turbulence at electron inertial scales is anisotropic and develops a very steep power-law spectrum which is consistent with recent solar wind observations. A comparison of the simulated spectrum with that predicted by a phenomenological turbulence scaling model suggests that the energy cascade at the electron inertial scale depends on both magnetic fluctuations and electron velocity fluctuations, as well as on the whistler dispersion relation. Thus, not only kinetic Alfven turbulence but also whistler turbulence may explain recent solar wind observations of very steep magnetic spectra at short scales.

OSTI ID:
21532084
Journal Information:
Physics of Plasmas, Vol. 17, Issue 12; Other Information: DOI: 10.1063/1.3526602; (c) 2010 American Institute of Physics; ISSN 1070-664X
Country of Publication:
United States
Language:
English