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Parts of the Algerian desert experienced massive thunderstorm clouds accompanied by heavy rains and hail showers, despite the region being one of the driest on Earth. This situation resulted from favorable atmospheric conditions for the development of thunderstorms, where upward air currents caused the clouds to grow vertically and reach high altitudes, with varying amounts of rain and hail falling. These storms often lead to the formation of floods in low-lying areas and valleys, creating a significant contrast between the desert's dry nature and these sudden weather phenomena.
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