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D region disturbances caused by electromagnetic pulses from lightning

Journal Article · · Geophysical Research Letters (American Geophysical Union); (United States)
DOI:https://doi.org/10.1029/92GL02379· OSTI ID:5238729

Electromagnetic pulses from weak lightning discharges (E[sub 100] = 1 V/m, where E[sub 100] is the field strength in the radiation pattern maximum at 100 km) may substantionally heat D region electrons, while only pulses with E[sub 100] [>=] 20 V/m may create electron density enhancements [>=]10% of ambient. A E[sub 100] = 20 V/m pulse from a horizontal radiator at 5 km altitude (e.g., the cloud discharge at the stepped-leader onset) increases the electron temperature by a factor of [approximately]400 maximum and the electron density (in one ionization cycle) by [approximately]230 cm[sup [minus]3] maximum; the widths at half-maximum of the heated and ionized regions are 200 km and 90 km. A E[sub 100] = 40 V/m pulse from a vertical radiator at 0 km altitude (e.g., the vertical return stroke channel) increases the electron temperature by a factor of [approximately]350 maximum and the electron density (in one ionization cycle) by [approximately]80 cm[sup [minus]3] maximum; the widths at half-maximum of the heated and ionized regions are 440 km and 260 km. Several ionization cycles should occur during a typical lightning pulse. 4 regs., 4 figs.

OSTI ID:
5238729
Journal Information:
Geophysical Research Letters (American Geophysical Union); (United States), Journal Name: Geophysical Research Letters (American Geophysical Union); (United States) Vol. 19:20; ISSN GPRLAJ; ISSN 0094-8276
Country of Publication:
United States
Language:
English

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