Using electric and magnetic field and field derivative sensors arrayed over an area of about 1 km2, we measured the close fields of stepped leaders and first return strokes in 18 negative cloud-to-ground lightning flashes at distances to individual sensors ranging from about 100 m to about 1 km. We present examples of the close field waveforms along with their statistical characterization as a function of the distance to the lightning. Statistical data are presented for the half-peak width of the stepped-leader/return-stroke electric field waveform; the stepped-leader electric field change; the return-stroke electric field change at 20, 100, and 1000 μs after return-stroke initiation; the peak electric field derivative; the risetime of the electric field derivative waveform; and the magnetic field initial peak, largest peak, risetime, and half-peak width. For example, in the 100–200 m range, the average half-peak width of the leader/return-stroke electric field change was about 0.8 ms; the average observed leader electric field change was about 40 kV m-1; the average return-stroke electric field change at 20 μs was about 35 kV m-1; and the average peak electric field derivative was about 15 kV m-1 μs-1, the largest unsaturated measurement being about 20 kV m-1 μs-1. Peak derivative values observed at close range are consistent with derivative measurements made for return strokes over salt water at distances of some tens of kilometers if an inverse-distance dependence is assumed for the field amplitude.
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