Rm. Thorne et Rb. Horne, MODULATION OF ELECTROMAGNETIC ION-CYCLOTRON INSTABILITY DUE TO INTERACTION WITH RING CURRENT O+ DURING MAGNETIC STORMS, J GEO R-S P, 102(A7), 1997, pp. 14155-14163
We demonstrate that the observed enhancement in the fractional composi
tion eta(O+) of ring current O+ ions during magnetic storms can have a
strong controlling effect on the excitation of electromagnetic ion cy
clotron (EMIC) waves. For modest storms, when eta(O+) less than or equ
al to 30%, strong EMIC excitation can occur in the frequency band abov
e the oxygen gryofrequency, Omega(O+), due to cyclotron resonance with
anisotropic ring current H+ ions. The path-integrated gain obtained f
rom ray tracing is sufficient to drive wave amplitudes into the nonlin
ear regime in a region near the equatorial duskside plasmapause. The e
xcited wave energy is found to be absorbed efficiently at high latitud
es via cyclotron resonant interactions with energetic O+ leading to pe
rpendicular heating of the O+ population. Intense waves generated near
the equator should therefore not be detectable at low altitudes once
the density of O+ has been enhanced during the main phase of a storm.
Cyclotron absorption will also enhance the anisotropy of energetic res
onant O+ ions. We show that such enhanced anisotropy can excite cyclot
ron instabilities at frequencies below Omega(O+) which are able to pro
pagate to low altitudes and be detectable either on the ground or on l
ow altitude satellites during the storm main phase. For the most inten
se storms, when the concentration of O+ can attain values eta(O+) grea
ter than or equal to 60%, cyclotron absorption by resonant O+ can beco
me so severe as to totally suppress wave excitation in the band above
Omega(O+). The most rapid loss process for the ring current (i.e., tha
t due to wave particle scattering) could therefore be suppressed durin
g the main phase of such storms. This raises the interesting question
of whether the main phase Dst depression might be modulated by the rel
ative concentration of energetic O+ through the process of resonant in
teraction with EMIC waves.