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Annales Geophysicae An interactive open-access journal of the European Geosciences Union
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Volume 17, issue 10
Ann. Geophys., 17, 1284–1292, 1999
https://doi.org/10.1007/s00585-999-1284-x
© European Geosciences Union 1999
Ann. Geophys., 17, 1284–1292, 1999
https://doi.org/10.1007/s00585-999-1284-x
© European Geosciences Union 1999

  31 Oct 1999

31 Oct 1999

Non-magnetic aspect sensitive auroral echoes from the lower E region observed at 50 MHz

R. Rüster and K. Schlegel R. Rüster and K. Schlegel
  • Max-Planck-Institut für Aeronomie, Katlenburg-Lindau, Germany

Abstract. Backscatter from E-region irregularities was observed at aspect angles close to 90° (almost parallel to the direction of the magnetic field) using the ALOMAR SOUSY radar at Andoya/Norway. Strong electric fields and increased E-region electron temperatures simultaneously measured with the incoherent scatter facility EISCAT proved that the Farley-Buneman plasma instability was excited. In addition, strong particle precipitation was present as inferred from EISCAT electron densities indicating that the gradient drift instability may have been active, too. Backscatter at such large aspect angles was not expected and has not been observed before. The characteristics of the observed echoes, however, are in many aspects completely different from usual auroral radar results: the Doppler velocities are only of the order of 10 m/s, the half-width of the spectra is around 5 m/s, the echoes originate at altitudes well below 100 km, and they seem to be not aspect-sensitive with respect to the magnetic field direction. We, therefore, conclude that the corresponding irregularities are not caused by the mentioned instabilities and that other mechanism have to be invoked.

Key words. Ionosphere (plasma waves and instabilities; ionosphere irregularities; particle precipitaion) · Meteorology and atmospheric dynamics (middle atmosphere dynamics)

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