During the Summer and Fall of 1998 we launched five balloon-borne instrumen
ts into thunderstorms to observe changes in the vertical component of elect
ric field caused by lightning. Four of these were for measurement of field
change only. The fifth was part of a larger package that included a gamma r
adiation detector and a GPS receiver on board. We have processed electric-h
eld-change data from two of these flights. We discuss examples of field cha
nges observed at altitude and compare them with data from the National Ligh
tning Detection Network (NLDN) for cloud-to-ground lightning flashes that w
ere coincident in time. Limits on time resolution and timing accuracy preve
nt unambiguous identification of the lightning processes that caused the fi
eld changes. It appears that they may have been caused by charge movements
relatively near the instruments as compared with the ground-strike location
of coincident flashes.