Attachment process in rocket-triggered lightning strokes

Citation
D. Wang et al., Attachment process in rocket-triggered lightning strokes, J GEO RES-A, 104(D2), 1999, pp. 2143-2150
Citations number
19
Categorie Soggetti
Earth Sciences
Volume
104
Issue
D2
Year of publication
1999
Pages
2143 - 2150
Database
ISI
SICI code
Abstract
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.