Journal of Geophysical Research Atmospheres · 2012 · 57 citations · 14 references
Natural SciencesElectrical EngineeringPhysicsAtmospheric ElectricityElectromagnetismPlasma PhysicsLightning CurrentLightning InitiationLightning PhysicsLightning PropagationThunderstorm ElectricityThunderstorm ElectrificationLightning Current MeasurementLightning Current WaveformsLightning Flash DurationLightning Initiation MechanismsPositive Lightning CurrentPositive Lightning FlashesStepped Leader DynamicsWeighted Arithmetic Mean
We report the measured current characteristics of positive lightning discharges to the Gaisberg Tower (GBT) in Austria from 2000 to 2009. On the basis of the recorded current waveforms, a total of 26 flashes consisting of initial stage only were identified as upward positive discharges initiated by an upward negative leader from GBT. They accounted for 4% (26/652) of the total flashes recorded at the GBT. Nineteen (73%) out of the 26 positive flashes occurred during nonconvective season (September–March). Median values of flash peak current, flash duration, charge transfer, and action integral were determined as 5.2 kA, 82 ms, 58 C, and 0.16 × 10 3 A 2 s, respectively. Current pulses of high repetition rate superimposed on the initial portion of initial continuous current are inferred to be associated with the upward negative stepped leader process. The weighted arithmetic means of leader pulse peak current, leader pulse duration, leader interpulse interval, and leader pulse charge are 3 kA, 31 μ s, 32 μ s, and 42 mC, respectively. On the basis of an assumed stepped leader speed in the range of 8 × 10 4 to 4.5 × 10 5 m/s an upward negative stepped leader channel charge density of 15–87 mC/m, a leader length of 168–945 m, and an average leader step length of 2.4–13.3 m were estimated. The upward negative stepped leader channel charge density and length are significantly larger and smaller than their counterparts in downward negative stepped leaders, respectively, while the upward leader step length is consistent with previous studies. Possible reasons for this are discussed.
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Positive leader characteristics from high‐speed video observations
Marcelo M. F. Saba, Kenneth L. Cummins, Tom A. Warner et al. · Geophysical Research Letters · 2008 · 187 citations · Full text