Leader Studies with the Los Alamos Sferic Array


M J Heavner, D A Smith, and A R Jacobson


LAUR-01-4198

LV/VLF & VHF Lightning Fast Stepped Leaders


This portion of the poster is based on "LF/VLF and VHF Lightning Fast Stepped Leader Observations" by Heavner, Smith, Jacobson, and Sheldon, which has been submitted to JGR.


The July 11, 2000 16:20:39.615019 UT event is presented below. FORTE's 100 MHz receiver triggered twice during the 8 ms LASA record, collecting two 546 us records. Panel a is the 8 ms Kennedy Space Center (KC) waveform overlaid with the two 546 us FORTE RF records. (scaled by 2.5 x 10 7). The sferic array located the event ~200 km east of the Florida coast, 309 km from the KC station. Also shown is an expanded view of the 546 us plot of FORTE power associated with the leader activity. Three pulse pairs are identified. Based on the delay between the direct and reflected pulses, the source heights are 5.3 km, 5.0 km, and 4.3 km as indicated. For time delays of 166.4 us and 119.3 us between the pairs of pulses, vertical velocities of 1.7 x 106 m/s and 5.4 x 106 m/s are determined. For the 285.7 us duration across all three pulse pairs, the average vertical velocity is 3.2 x 106 m/s.
FORTE/LASA waveforms

We have identified a total of four intense/fast leader events for which heights and velocities may be determined. These leaders associated with inital return strokes have average vertical velocity 2.1 x 106 m/s, with a range in velocities of 0.88 - 5.4 x 106 m/s. The leader step altitudes are between 4.0-5.5 km. The multiple-step velocity determination is consistent with the velocity required for the leader propagation from the initial height to the ground in the time between the initial leader and the return stroke. One important issue regarding these observations is whether the observed leader is from an initial or subsequent return stroke (to understand if the leader is a stepped leader or dart leader), based on evidence discussed by Heavner et al, 2002, submitted the events are initial return strokes.


Below, we illustrate the geometry for altitude determination us FORTE. Given satellite and 2-D source positions, the relative delay provides the source altitude (Jacobson et al, 1999).

LASA/FORTE Geometry

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Los Alamos National Laboratory