Electron precipitation

Electron precipitation (also called energetic electron precipitation or EEP) is an atmospheric phenomenon that occurs when previously trapped electrons enter the Earth's atmosphere, thus creating communications interferences and other disturbances.[1] Electrons trapped by Earth's magnetic field spiral around field lines to form the Van Allen radiation belt. The electrons are from the solar wind and may remain trapped above Earth for an indefinite period of time (in some cases years). When broadband very low frequency (VLF) waves propagate the radiation belts, the electrons exit the radiation belt and "precipitate" (or travel) into the ionosphere (a region of Earth's atmosphere) where the electrons will collide with ions.[2] Electron precipitation is regularly linked to ozone depletion. It is often caused by lightning strikes.

  1. ^ "Ground Observations of Lightning-Induced Electron Precipitation | Stanford VLF Group". vlf.stanford.edu. Retrieved 2015-10-19.
  2. ^ Voss, H. D.; Imhof, W. L.; Walt, M.; Mobilia, J.; Gaines, E. E.; Reagan, J. B.; Inan, U. S.; Helliwell, R. A.; Carpenter, D. L. (1984-12-20). "Lightning-induced electron precipitation". Nature. 312 (5996): 740–742. Bibcode:1984Natur.312..740V. doi:10.1038/312740a0. S2CID 4302334.

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