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VOLUME 24 (1976) | ISSUE 10 | PAGE 558
Strong Langmuir turbulence in the earth's magnetosphere as a source of kilometer radio emission
The source of the earth's radio emission is taken in this paper to be the strong Langmuir turbulence excited by a beam of electrons that spill out of the tail of the earth's magnetosphere, followed by a reradiation of their energy at double the plasma frequency. The obtained efficiency of this conversion is capable of ensuring an observable effectiveness of the radiation.