C. Lathuillere et al., ANALYSIS OF F-REGION INCOHERENT-SCATTER SPECTRA DURING PERIODS OF HIGH ELECTRIC-FIELDS, Journal of Geomagnetism and Geoelectricity, 47(9), 1995, pp. 861-868
In the presence of high electric fields in the auroral ionosphere, the
ion distribution functions depart from their usual Maxwellian shape.
The incoherent scatter radars have observed the signature of this phen
omenon in the form of distorted spectra which have lost their double-h
umped characteristics. In consequence, the classical procedure of spec
trum analysis, which assumes Maxwellian distributions to fit the plasm
a parameters, is no longer valid and has to be modified to account for
a non-Maxwellian plasma. The observations of the European incoherent
scatter radar EISCAT were at the origin of substantial developments, w
hich are still in progress. We briefly review the main steps in the ex
perimental and theoretical approaches of the non-Maxwellian behaviour
of the ionospheric plasma, and we discuss particularly the most recent
ly published results.