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Waves from whistlers

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In the auroral region, solitary plasma waves form in a low-density plasma when energetic electron beams hit and energize ambient ions to escape velocity. Electromagnetic waves from lightning trigger similar plasma behaviour in the equatorial ionosphere.

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Figure 1: Ionospheric turbulence.

References

  1. Berthelier et al. Nature Geosci. 2, 101–105 (2008).

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  2. Kelley et al. Geophys. Res. Lett. 17, 2221–2224 (1990).

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Kelley, M. Waves from whistlers. Nature Geosci 1, 93–94 (2008). https://doi.org/10.1038/ngeo112

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