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- W2051490664 abstract "Laboratory studies of charge transfer, when vapor‐grown ice crystals bounce off a hailstone in simulated thunderstorm conditions, have shown that the sign and magnitude of the charge separated is a sensitive function of the cloud and cloud particle properties. In general, at temperatures colder than −20°C, hail becomes negatively charged, but at warmer temperatures it becomes positively charged. The formation of the lower positive charge center in thunderstorms and the initiation of a lightning flash which precedes the commonly observed gush of rain on the ground may be explained in terms of this charging process." @default.
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- W2051490664 date "1984-12-20" @default.
- W2051490664 modified "2023-10-09" @default.
- W2051490664 title "The “rain gush”, lightning, and the lower positive charge center in thunderstorms" @default.
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- W2051490664 doi "https://doi.org/10.1029/jd089id07p11816" @default.
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