We performed a statistical study on the initial stage (IS) of negative rock
et-triggered lightning using 37 channel-base current recordings obtained du
ring the summer of 1994 at Fort McClellan, Alabama, and during the summers
of 1996 and 1997 at Camp Blanding, Florida. The IS can be viewed as compose
d of an upward positive leader (UPL) followed by an initial continuous curr
ent (ICC). The IS has a geometric mean (GM) duration of 279 ms and lowers a
GM charge of 27 C to the ground. The average IS current in an individual l
ightning discharge varies from a minimum of 27 A to a maximum of 316 A with
a GM value of 96 A for the entire sample of 37 discharges. We examined the
current variation at the beginning of the IS in 24 flashes. In 22 out of 2
4 cases this initial current variation (ICV) includes a current drop, proba
bly associated with the disintegration of the copper triggering wire and th
e subsequent current reestablishment. The GM time interval between the onse
t of the initial stage and the abrupt decrease in current is 8.6 ms, and th
e GM current level just prior to the current decrease is 312 A, a value abo
ut 3 times the GM value of average current for the whole IS, 96 A. Before t
his abrupt current decrease, a GM charge of 0.8 C has been lowered to groun
d with a corresponding GM action integral of 110 A(2) s. The abrupt current
decrease takes typically several hundred microseconds and is followed, imm
ediately or after a time interval up to several hundred microseconds, by a
pulse with a typical peak of about 1 kA and a typical risetime of less than
100 mu s. The ICC usually includes impulsive processes that resemble the M
processes observed during the continuing currents that follow return strok
es in both natural and triggered lightning. We present statistics for the f
ollowing parameters of current pulses superimposed on the ICC: magnitude, r
isetime, half-peak width, duration, charge transferred, preceding continuou
s current level, interpulse interval, and time interval between the onset o
f the IS and the first ICC pulse. The observed characteristics of ICC pulse
s varied significantly among the three data sets. For all data combined, th
e characteristics of the ICC pulses are similar to those of the M-component
current pulses studied by Thottappillil et al. [1995]. This latter finding
suggests that ICC impulsive processes are of the same nature as M processe
s.