Presented are the first known vertical profiles of electric field, E, in six winter nimbostratus clouds in the USA. No lightning was detected while the E profiles were collected. Deep convection was embedded in one of the clouds that had been a thunderstorm. The maximum magnitude of the vertical component of the electric field, E z , in the profiles ranged from 1 to 12 kV m −1 ; the maximum horizontal component ranged from 0.2 to 28 kV m −1 . The latter indicates that the charge in the cloud was not horizontally homogeneous. The E z versus altitude profiles have 1–3 peaks inside the clouds. From the profiles, we inferred up to four charge regions stacked vertically. Peaks in E z are found in regions of melting as evidenced by radar bright bands: Both polarities of charge are inferred in the bright bands. Three nimbostratus clouds without melting precipitation also were electrified.
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Rust et al. (2002) studied this question.
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