In order to study the lightning attachment process, we have obtained highly
resolved (about 100 ns time resolution and about 3.6 m spatial resolution)
optical images, electric field measurements, and channel-base current reco
rdings for two dart leader/ireturn-stroke sequences in two lightning flashe
s triggered using the rocket-and-wire technique at Camp Blanding, Florida.
One of these two sequences exhibited an optically discernible upward-propag
ating discharge that occurred in response to the approaching downward-movin
g dart leader and connected to this descending leader. This observation pro
vides the first direct evidence of the occurrence of upward connecting disc
harges in triggered lightning strokes, these strokes being similar to subse
quent strokes in natural lightning. The observed upward connecting discharg
e had a light intensity one order of magnitude lower than its associated do
wnward dart leader, a length of 7-11 m, and a duration of several hundred n
anoseconds. The speed of the upward connecting discharge was estimated to b
e about 2 x 10(7) m/s, which is comparable to that of the downward dart lea
der. In both dart leader/return-stroke sequences studied, the return stroke
was inferred to start at the point of junction between the downward dart l
eader and the upward connecting discharge and to propagate in both upward a
nd downward directions. This latter inference provides indirect evidence of
the occurrence of upward connecting discharges in both dart leader/return-
stroke sequences even though one of these sequences did not have a discerni
ble optical image of such a discharge. The length of the upward connecting
discharges (observed in one case and inferred from the height of the return
-stroke starting point in the other case) is greater for the event that is
characterized by the larger leader electric field change and the higher ret
urn-stroke peak current. For the two dart leader/return-stroke sequences st
udied, the upward connecting discharge lengths are estimated to be 7-11 m a
nd 4-7 m, with the corresponding return-stroke peak currents being 21 kA an
d 12 kA, and the corresponding leader electric field changes 30 m from the
rocket launcher being 56 kV/m and 43 kV/m. Additionally, we note that the d
ownward dart leader light pulse generally exhibits little variation in its
10-90% risetime and peak value over some tens of meters above the return-st
roke starting point, while the following return-stroke light pulse shows an
appreciable increase in risetime and a decrease in peak value while traver
sing the same section of the lightning channel. Our findings regarding (1)
the initially bidirectional development of return-stroke process and (2) th
e relatively strong attenuation of the upward moving return-stroke light (a
nd by inference current) pulse over the first some tens of meters of the ch
annel may have important implications for return-stroke modeling.