A new quasi-electrostatic model of high altitude electric field generation due to the lightning - induced change of a thundercloud electric structure is presented. The key point of the model is the assumption that a highly conducting channel arises due to a cloud - to - ground (CG) discharge, which brings the ground potential to a region near the cloud bottom in some tens of milliseconds after the discharge initiation. Substantial increase in the electric field strength above the thundercloud at this moment is found. A horizontal extension of the lightning channel is taken into account in the framework of the bidirectional model of the channel propagation. This geometry provides a substantially bigger electric field perturbation than the simplest geometry of the vertical lightning channel does.
CITATION STYLE
Smirnova, E. I., Mareev, E. A., & Chugunov, Y. V. (2000). Modeling of lightning generated electric field transitional processes. Geophysical Research Letters, 27(23), 3833–3836. https://doi.org/10.1029/1999GL011158
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