At. Weatherwax et al., STATISTICAL AND CASE-STUDIES OF RADIO EMISSIONS OBSERVED NEAR 2F(CE) AND 3F(CE) IN THE AURORAL-ZONE, J GEO R-S P, 100(A5), 1995, pp. 7745-7757
Receivers located at Two Rivers, Alaska (64.9 degrees N, 146.9 degrees
W), and Circle Hot Springs, Alaska (65.5 degrees N, 144.7 degrees W),
have been used to monitor the spectrum between 0.05-4.8 MHz for exten
ded periods. Seasonal and diurnal effects of auroral roar, a weak narr
ow band radio emission near 2 and 3 times the ionospheric electron cyc
lotron frequency (f(ce)), have been determined. Many individual aurora
l roar events correlate with magnetic activity, and superposed epoch a
nalysis using planetary K indices shows a correlation between magnetic
activity and auroral roar commencement. For a 3f(ce) roar event on Ma
rch 23, 1992, riometer, magnetometer, photometer, and all-sky camera d
ata are available and show that individual bursts of 3f(ce) auroral ro
ar are associated with intensifications of the aurora, as was known pr
eviously for 2f(ce) roar. Finally, two possible generation mechanisms
are investigated in detail: nonlinear interaction between lower hybrid
and electrostatic upper hybrid waves producing electromagnetic waves,
and the feasibility of a lower ionospheric decameter maser for direct
generation of X mode waves at harmonics of f(ce).