Severe thunderstorm development occurs independently from the air flow aloft.

Name: Severe thunderstorm development occurs independently from the air flow aloft.
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Severe thunderstorm development is dependent on a variety of factors, including an unstable atmosphere, wind shear (changes in wind speed and direction with height), moisture, and lifting mechanisms. The air flow aloft can play a significant role in thunderstorm development, helping to provide additional uplift and instability.

Severe Thunderstorm Development Occurs Independently from the Air Flow Aloft