The downdraft of a thunderstorm can be described as a pocket of descending air that is loaded with precipitation from the storm. This pocket of air is cold as it falls from the clouds.
A storm that generates lighting and thunder is called a thunderstorm. Some thunderstorms don't bring on any precipitation. The majority of thunderstorms fall into the single cell category since they are not usually severe. Fortunately, supercells and mesoscale convective complexes, which produce the most damaging thunderstorms, are exceedingly infrequent. These storms are highly complicated, and their causes are not entirely known.
More air from above will descend as a result of falling air parcels that get colder (and denser) than the ambient air around them. A downdraft is the term used to describe the rapidly falling air that has been cooled by evaporation. The air in the downdraft is cooler than the air around it. Downdrafts are a common byproduct of thunderstorms, and under the correct circumstances they may be highly powerful and devastating.
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