Towering cumulonimbus clouds are a common feature in regions where moist unstable air is heated from below.Such clouds are produced by

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Towering cumulonimbus clouds are formed due to convectional lifting of moist and unstable air. As the air is heated from below, it rises and cools, which causes the moisture to condense and form clouds. This process is commonly observed in tropical regions where the warm sea surface temperature provides the necessary heat for convectional lifting to occur.

Towering Cumulonimbus Clouds Are a Common Feature in Regions Where