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On the plasma environment of solitary waves and weak double layers

Journal Article · · Journal of Geophysical Research; (United States)
 [1];  [2];  [3]
  1. Finnish Meteorological Inst., Helsinki (Finland)
  2. Swedish Inst. of Space Physics, Kiruna (Sweden)
  3. Swedish Inst. of Space Physics, Uppsala (Sweden)
Observations of charged particles during events of solitary waves and weak double layer-like structures by the Swedish magnetospheric research satellite Viking are discussed. The observations took place in relatively weak acceleration regions at altitudes between 1 and 2 R{sub E}. The total accelerating potential was typically somewhat less than 1 kV. The characteristics of ion and electron spectra indicate that the main part of the potential was below the satellite but osme field-aligned acceleration of elections had also taken place above it. The composition of the ion beams was domianted by protons with a variable concentration (0-30%) of oxygen ions. While it is difficult to determine the exact parameters of the background plasma, there is clear evidence of the presence of cool background electrons and ions. It is proposed that the weak double layer-like structures are structures in the cool ambient ions and convect slowly upward with the ion population. On the other hand, the structures accelerate auroral electrons toward Earth and beam ions from the ionosphere upward. It is suggested that the structures are likely to contribute to the perpendicular heating of the ion beams.
OSTI ID:
5029014
Journal Information:
Journal of Geophysical Research; (United States), Journal Name: Journal of Geophysical Research; (United States) Vol. 95:A5; ISSN 0148-0227; ISSN JGREA
Country of Publication:
United States
Language:
English