Bj. Fraser et al., CRRES POYNTING VECTOR OBSERVATIONS OF ELECTROMAGNETIC ION-CYCLOTRON WAVES NEAR THE PLASMAPAUSE, J GEO R-S P, 101(A7), 1996, pp. 15331-15343
Electromagnetic ion cyclotron waves have been observed by the Air Forc
e Geophysics Laboratory triaxial fluxgate magnetometer on the CRRES sa
tellite in the vicinity of the plasmapause. Specific wave events in th
e 1300-0100 MLT local time sector and over L = 4.8 - 6.7 at magnetic l
atitudes between +/- 20 degrees have been studied with respect to ener
gy propagation. Using the wave magnetic field data and the orthogonal
two-component Berkeley electric field experiment data allows the compu
tation of the Poynting vector. Nine events with frequencies below 0.6
Hz have been analyzed. General wave properties showed intensities in t
he range 4 - 18 mu W m(-2). In most events, energy propagation was pre
dominantly away from the equator, supporting the existence of an equat
orial source region. There are exceptions and one event, observed 3 de
grees from the equator, also showed some propagation back to the equat
or with equal energy. Four periodic wave packets were seen in another
event. This event showed unidirectional propagation away from the equa
tor over all packets with periodicity approximately one-half of the ca
lculated time for a typical bouncing wave packet. Consequently, the pe
riodicity is not the signature of a classical periodic structured Pc 1
-2 pulsation event of the type seen on the ground. Generally, the resu
lts for these waves with f < f(He)+ may be interpreted by assuming an
ion cyclotron instability source located near the equator and irregula
rly emitting wave trains of energy into one or both hemispheres, with
minimal reflection at the ionosphere.