Re. Erlandson et al., SIMULTANEOUS OBSERVATIONS OF SUBAURORAL ELECTRON-TEMPERATURE ENHANCEMENTS AND ELECTROMAGNETIC ION-CYCLOTRON WAVES, Geophysical research letters, 20(16), 1993, pp. 1723-1726
Observational results from an investigation of low frequency (0.5-4.0
Hz) electromagnetic ion cyclotron waves and subauroral electron temper
ature enhancements recorded from the DE-2 satellite are presented. Fou
r different wave events were analyzed, all recorded at magnetic latitu
des from 57-60-degrees, magnetic local times from 8-14 hours, and alti
tudes from 600-900 km. The peak wave amplitudes during the events rang
ed from 870 nT and 5-30 mV/m in the magnetic and electric field, respe
ctively. Electron temperature (T(e)) enhancements at the time of the w
aves were observed in 3 of 4 events. A linear relationship between the
wave magnetic field spectral density and T(e) enhancements was found
for these events. The T(e) enhancements were also correlated with an e
nhanced flux of low energy electrons. During one event (82104) an enha
nced flux of electrons were observed at energies up to 50eV and at nea
rly all pitch angles, although the flux was largest in the precipitati
ng and upflowing directions. It is suggested that the waves are respon
sible for heating the low energy electrons which precipitate to the io
nosphere and produce the observed T(e) enhancements. The upflowing ele
ctron population appears to be heated at ionospheric altitudes, below
the DE-2 satellite. The precipitating electrons may also be heated at
ionospheric altitudes through Landau damping, although the observation
s do not rule out electron heating near the equator.