Data obtained from the Australia Wide Array of Geomagnetic Stations (A
WAGS) have provided a unique opportunity to investigate the spatial va
riation of long-period (Pc 5) ULF wave signal characteristics as a res
ult of plasma waves in low latitudes. Pure state filtering techniques
were applied in order to detect highly polarized Pc5 events and derive
the wave signal parameters, i.e., the wave frequency, amplitude, pola
rization, and phase. The results indicate that the Pc 5 signal frequen
cy was virtually independent of latitude and longitude, while the ampl
itude decreased considerably toward lower latitudes. The spatial varia
tion of the signal polarization was found to be small. However, a stat
istical analysis of the signal polarization revealed a systematic diur
nal variation. Counterclockwise sense of rotation (viewed in the direc
tion of the ambient magnetic field) with the major axis of the polariz
ation ellipse in the northeast quadrant was observed in the local morn
ing, while clockwise sense of rotation with the polarization major axi
s aligned mainly in the north-south direction was seen in the local af
ternoon. Interstation phase analysis yielded small phase variations ac
ross the entire station array, indicating azimuthal wave numbers of 1
< m < 3. The signals appeared to propagate westward in the local morni
ng sector, while eastward propagation prevailed in the local afternoon
. The latitudinal phase variation was also very small, showing signals
virtually in phase or with the lower-latitude stations leading slight
ly. These observations appear to be consistent with the magnetic groun
d signature of global compressional modes or large scale-cavity resona
nces trapped in the magnetosphere.