K. Stasiewicz et al., WAVE ENVIRONMENT INSIDE AN INVERTED-V ELECTRON EVENT OBSERVED BY FREJA, Geophysical research letters, 21(17), 1994, pp. 1839-1842
We present an analysis of the wave environment observed inside an inve
rted-V electron event at an altitude of 1700 km, occurring in the upwa
rd directed current with intensity of a few muAm-2. During the analyze
d event we observe that precipitating auroral electrons (approximately
2 keV) generate intense (40 mV/m) auroral hiss with peak power concen
trated at the lower hybrid frequency f(lh) almost-equal-to f(pi), and
weak Langmuir waves at f(pe). The low frequency turbulence observed wi
thin the event is found to be composed of a mixture of Alfven waves, O
+ cyclotron waves, multi-ion resonances, and ion sound waves. The LH w
aves appear to interact modulationally with O+ and ion sound waves. Fr
om the observed values Of f(lh) and multi-ion resonance frequencies it
is possible to estimate three-ion composition of plasma with represen
tative values of [23, 19, 58] percent for normalized number densities
of [H+, He+, O+], respectively.