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Other causes have additionally been proposed, counting on electrodynamic effects of the enormous current performing on the plasma in the bolt of lightning. Scientists have agreed since the 20th century that thunder should begin with a shock wave in the air due to the sudden thermal growth of the plasma in the lightning channel. In an inversion, the air near the bottom is cooler than the higher air; inversions typically occur when heat moist air passes above a chilly front. Inversion thunder results when lightning strikes between cloud and floor happen throughout a temperature inversion; the ensuing thunder sounds have considerably higher acoustic power than from the identical distance in a non-inversion condition. Cloud-to-floor lightning (CG) sometimes consists of two or extra return strokes, from floor to cloud. The most noticeable aspect of lightning and thunder is that the lightning is seen before the thunder is heard. National Lightning Safety Institute. NOAA National Severe Storms Laboratory.
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