We analyze the ROCSAT-1 IPEI data collected between March and June 1999 to
study the statistical features of the ion vertical drifts at equatorial and
tropical latitudes. The dependencies of ion vertical drifts on local time,
longitude and geomagnetic field configuration, as well as geomagnetic acti
vity are examined. The variations of the equatorial vertical drifts near th
e dawn and dusk terminators are of particular interest. From this prelimina
ry study, we have shown that the overall local-time characteristics of the
quiet-time equatorial vertical drift patterns derived from IPEI are in good
agreement with those observed by other satellites and groundbased instrume
nts. More importantly, several new results due to the unique 35 degrees orb
ital inclination of ROCSAT-1 and the 100% duty-cycle operation of IPEI are
found. These include: (a) enhanced upward ion drifts to a critical level of
30-60 m/s at post-sunset hours strongly correlate with the occurrence of r
ising bubbles in the pre-midnight local time sector; (b) large (> 300 m/s)
downward ion drifts are most often found near sunrise and at longitudes whe
re the geomagnetic field has greatest variations; (c) the statistical drift
patterns strongly depend on the hemispheres at the equatorial anomaly lati
tudes, This north-south asymmetry may result from seasonal effects and/or f
rom differences in geomagnetic field configuration.