A two-dimensional electromagnetic particle-in-cell simulation in a magnetized, homogeneous, collisionless plasma of electrons and protons has been carried out, demonstrating a forward cascade of whistler turbulence. Enhanced magnetic fluctuation spectra are initially imposed with -0.2 < 0.2 and -0.2 < 0.2 where the directional subscripts denote directions relative to the background magnetic field Bo and c/ωe is the electron inertial length. The late-time evolution of the simulation shows a cascade of magnetic fluctuation energy to shorter wavelengths; furthermore, the spectrum is anisotropic with more fluctuation energy at a given wavenumber perpendicular to Bo than at the same wavenumber parallel to the background field. The late-time electron velocity distribution shows a magnetic-field aligned signature due to the Landau resonance of the obliquely propagating whistlers. Copyright 2008 by the American Geophysical Union.
CITATION STYLE
Gary, S. P., Saito, S., & Li, H. (2008). Cascade of whistler turbulence: Particle-in-cell simulations. Geophysical Research Letters, 35(2). https://doi.org/10.1029/2007GL032327
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