Abstract:
The vertical E B drift is very important parameter as its day to day variability has great influence on the variability in the low latitude
F-region ion and electron density distributions. The measurements of vertical ion velocity from the first Republic of China Satellite
(ROCSAT-1) provide a unique data base for the development of possible relationship between vertical E B drifts and ground based
magnetometer observation. An attempt has been made to derive quantitative relationship between F-region vertical E B drifts
measured by ROCSAT-1 (600 km) and ground measured equatorial electrojet for the solar maximum period 2001–2003 for Indian
and Japanese sectors. The results consistently indicate existence of linear relationship between the measured vertical E B drifts at topside
F-region and EEJ for both the sectors, with a moderate to high correlation coefficients. The linear relationship between ROCSAT-1
measured E B drifts and EEJ for Indian and Japanese sectors has been compared with a similar relationship with Jicamarca Unattended
Long-term Ionosphere Atmosphere Radar (JULIA) measured E B drifts (150 km echos) and EEJ strength from Peruvian sector
during 2003. It has been found that ROCSAT-1 measured E B drifts shows linear relationship with EEJ, however, exhibits a larger
scatter unlike JULIA radar observed E B drifts. This may be attributed to the large height difference as ROCSAT-1 measures E B
drifts at 600 km altitude and the EEJ is E-region (110 km) phenomenon.
