Fleeting columns of luminosity occurring above large thunderstorms at
50-90 km altitude, presently known as sprites, were imaged with an int
ensified video charge coupled device (CCD) camera during a July 1995 g
round-based campaign near Fort Collins, Colorado. These unfiltered int
ensified images reveal detailed spatial structure within the sprite en
velope. The temporal resolution of standard interlaced video imagery i
s limited by the 60 fields per second acquisition rate (16 ms). The sp
ecific CCD used here, however, is subject to bright events leaking int
o the readout registers, allowing time-resolution on the order of the
linescan rare (63 mu s). Typical sprite onset is found to follow the a
ssociated cloud lightning by 1.5 to 4 ms. The onsets of the individual
sprites within a cluster are generally, but not always, simultaneous
to within 1 ms. Sprites tend to have a bright localized core, less tha
n 2 km in horizontal dimension, which rises to peak intensity within 0
.3 ms and maintains this level for 5 to 10 ms before fading over an ad
ditional 10 ms.