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A self consistent and fully kinetic simulation of the interaction of lightning radiated electromagnetic (EM) pulses with the nighttime lower ionosphere indicates that optical emissions observable with conventional instruments would be excited. For example, emissions of the 1st and 2nd positive bands of N 2 occur at rates reaching 7 × 10 7 and 10 7 cm −3 s −1 respectively at ∼92 km altitude for a lightning discharge with an electric field E 100 = 20 V/m (normalized to a 100 km distance). The maximum height integrated intensities of these emissions are 4 × 10 7 and 6 × 10 6 R respectively, lasting for ∼50 µs.
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Taranenko et al. (1993) studied this question.
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