An analysis of concurrent Pc 1 pulsation activity (0.2-0.6 Hz) recorde
d on the ground at Mawson, Antarctica (70 degrees 8 magnetic latitude
(MLAT); 19 degrees E magnetic longitude (MLONG); L=8), acid on board t
he Viking polar-orbiting satellite, when the spacecraft was located ne
ar apogee (13.5x10(3) km) from 50-77 degrees MLAT above the northern i
onosphere, shows that simultaneous pulsations were observed only when
Viking's conjugate point was within 60-70 degrees S MLAT and 30 degree
s E-33 degrees W MLONG, an extent of about 1000 km in latitude and 170
0 km in longitude. Spectral analysis confirms that the waves responsib
le for these pulsations are electromagnetic ion cyclotron (EMIC) waves
that have propagated to the spacecraft and ground from the geomagneti
c equates. For the intervals when the waves were on field lines above
and equatorward of Mawson, convective EMIC wave modeling shows wave gr
owth is dominant below the equatorial He+ gyrofrequency. Waves generat
ed on field lines poleward of Mawson exhibit frequencies above the equ
atorial He+ gyrofrequency. These propagate to Mawson, most likely thro
ugh a purely proton plasma rather than a multi-ion environment. Freque
ncy shifts in the Pc 1 activity at Mawson appear to be directly linked
to solar wind velocity and flux variations measured by IMP 8. For cer
tain intervals these linked observations are consistent with an interp
retation based on the velocity and flux changes altering the radial po
sition of the magnetopause through pressure balance considerations. Th
is, in turn, changes the magnitude of the ambient magnetic field in th
e equatorial plasma trough and consequently the ion gyrofrequency and
EMIC growth rate. Pc 3-5 activity was recorded at Mawson in conjunctio
n with the Pc 1 frequency shifts and in association with rapid B-IMF v
ariations. The changes in the temperature anisotropy and energy of the
resonant ions in the plasma trough, which are causing the Pc 1 emissi
on changes, are associated with the entry of dayside Pc 3-5 pulsation
energy into the dayside magnetosphere.