Global observations of the auroral x-ray emissions during three large magne
tic storms in 1998 are presented from the Polar Ionospheric X-ray Imaging E
xperiment (PIXIE). The cross-polar-cap potential drop (Delta Phi (PC)) rema
ined large (> 100 kV) throughout most of the stormtime periods, and most of
the x-ray emissions observed were associated with enhanced earthward conve
ction and dawnward drift of electrons caused by substantial cross-tail elec
tric fields. Large increases in Delta Phi (PC) drove impulsive disturbances
termed convection enhancements that showed signatures inconsistent with su
bstorm activity, including substantial auroral emissions in the morning sec
tor and Little activity in the premidnight sector.