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    Cumulonimbus clouds are also known as thunderheads due to their unique mushroom shape. These clouds often produce lightning in their heart, which is caused by ionized droplets in the clouds rubbing against each other. The water vapor in the lower portions of the cumulonimbus becomes ice crystals, such as snow and graupel, the interaction of which can lead to hail and to lightning formation, respectively. The average duration of a lightning strike is 0.52 seconds, but it consists of a series of shorter strokes each lasting between 60 and 70 microseconds. On average, a lightning strike releases a gigajoule of energy and heats air to temperatures five times hotter than the surface of the Sun.
     
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