A laboratory investigation of Alfvén wave refraction in a parallel \bar\beta gradient

Physics – Plasma Physics

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Space Plasma Physics: Laboratory Studies, Magnetospheric Physics: Storms And Substorms, Magnetospheric Physics: Plasma Waves And Instabilities, Magnetospheric Physics: Auroral Phenomena (2407), Space Plasma Physics: Waves And Instabilities

Scientific paper

We present a laboratory investigation of Alfvén wave refraction due to a gradient in the plasma beta along the magnetic field. Theoretically, it is expected that perpendicular wave refraction occurs when the Alfvén wave changes from kinetic to inertial, as occurs along a typical auroral field line. The change in propagation characteristics is expected to produce a focusing of the wave energy. In the Earth's magnetosphere it is thought that this refractive property may play a key role in the field line resonance process. This effect is observed in the laboratory by creating a plasma with a parallel \bar{\beta} gradient of 100 per 105 Debye lengths. An Alfvén wave is then launched with an antenna, and the B field patterns of the wave are observed at several axial locations.

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