Energetic protons having ring type distributions are shown to generate
low-frequency electrostatic waves, propagating nearly transverse to t
he geomagnetic field lines, in the ring current region by exciting Mod
e 1 and Mode 2 nonresonant instabilities and a resonant instability. M
ode 1 nonresonant instability has frequencies around similar to 4 Hz w
ith transverse wavelengths of similar to(8-80) km, and it is likely to
occur in the region L = (7-8). Mode 2 nonresonant instability can gen
erate frequencies similar to(850-1450) Hz with transverse wavelengths
similar to(2-20) km. The typical frequencies and transverse wavelength
s associated with the resonant instability are (950-1250) Hz and (30-6
5) km. Both the Mode 2 nonresonant instability and the resonant instab
ility can occur in the ring current region with L = (4-6). The low-fre
quency modes driven by energetic protons could attain maximum saturati
on electric field amplitude varying from 0.8 mV/m to 70 mV/m. It is su
ggested that the turbulence produced by the low-frequency modes may ca
use pitch angle scattering of ring current protons in the region outsi
de the plasmapause resulting in the ring current decay.