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Proceedings of the Indian Academy of Sciences - Section A, 1943
The development of a thunderstorm which is essentially a convective phenomenon needs a cause for initial convection and then conditions for its maintenance once started. The possibility of the inherent instability due to potentially colder air superposed on potentially warmer air or the analogous case of extra injection of moisture in the lower layers ...
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The development of a thunderstorm which is essentially a convective phenomenon needs a cause for initial convection and then conditions for its maintenance once started. The possibility of the inherent instability due to potentially colder air superposed on potentially warmer air or the analogous case of extra injection of moisture in the lower layers ...
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Notes and Queries, 1891 Thundercells and Thunderstorms
1993Most lightning activity in North America is the result of a separation of electrical charges due to air turbulence created when a summertime cold front from the north collides with a warm air mass sweeping up from the south. The “frontal” or “squall line” storms thus created are large-scale events whose turbulent fronts may extend several hundred miles,
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The electrification of thunderstorms
Quarterly Journal of the Royal Meteorological Society, 1981openaire +2 more sources