WAVE ENVIRONMENT INSIDE AN INVERTED-V ELECTRON EVENT OBSERVED BY FREJA

Citation
K. Stasiewicz et al., WAVE ENVIRONMENT INSIDE AN INVERTED-V ELECTRON EVENT OBSERVED BY FREJA, Geophysical research letters, 21(17), 1994, pp. 1839-1842
Citations number
17
Categorie Soggetti
Geosciences, Interdisciplinary
ISSN journal
00948276
Volume
21
Issue
17
Year of publication
1994
Pages
1839 - 1842
Database
ISI
SICI code
0094-8276(1994)21:17<1839:WEIAIE>2.0.ZU;2-X
Abstract
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.