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Annales Geophysicae An interactive open-access journal of the European Geosciences Union
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Volume 20, issue 6
Ann. Geophys., 20, 863-870, 2002
https://doi.org/10.5194/angeo-20-863-2002
© Author(s) 2002. This work is distributed under
the Creative Commons Attribution 3.0 License.
Ann. Geophys., 20, 863-870, 2002
https://doi.org/10.5194/angeo-20-863-2002
© Author(s) 2002. This work is distributed under
the Creative Commons Attribution 3.0 License.

  30 Jun 2002

30 Jun 2002

Some features of stepped and dart-stepped leaders near the ground in natural negative cloud-to-ground lightning discharges

X. Qie1, Y. Yu1, C. Guo1, P. Laroche2, G. Zhang1, and Q. Zhang1 X. Qie et al.
  • 1Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou, Gansu 730000, P. R. China
  • 2Office National d’Etudes et de Recherche Aerospatiales, Chatillon, France
  • Correspondence to: X. Qie (qiex@ns.lzb.ac.cn)

Abstract. Characteristics of the electric fields produced by stepped and dart-stepped leaders 200 µs just prior to the return strokes during natural negative cloud-to-ground (CG) lightning discharges have been analyzed by using data from a broad-band slow antenna system with 0.08 µs time resolution in southeastern China. It has been found that the electric field changes between the last stepped leader and the first return stroke could be classified in three categories. The first type is characterized by a small pulse superimposed on the abrupt beginning of the return stroke, and accounts for 42% of all the cases. The second type accounts for 33.3% and is characterized by relatively smooth electric field changes between the last leader pulse and the following return stroke. The third type accounts for 24.7%, and is characterized by small pulses between the last recognizable leader pulse and the following return stroke. On the average, the time interval between the successive leader pulses prior to the first return strokes and subsequent return strokes was 15.8 µs and 9.4 µs, respectively. The distribution of time intervals between successive stepped leader pulses is quite similar to Gaussian distribution while that for dart-stepped leader pulses is more similar to a log-normal distribution. Other discharge features, such as the average time interval between the last leader step and the first return stroke peak, the ratio of the last leader pulse peak to that of the return stroke amplitude are also discussed in the paper.

Key words. Meteology and atmospheric dynamics (atmospheric electricity; lightning) – Radio science (electromagnetic noise and interference)

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