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A mesocyclone is a rapidly rotating column of air within a thunderstorm that can lead to tornado formation. These rotating updrafts are typically 10 to 20 km (6 to 12 miles) in diameter and form at altitudes of 4 to 8 km (2.5 to 5 miles).12

The formation of a mesocyclone requires specific atmospheric conditions, including moist, unstable air near the surface and cooler, drier air at higher levels. Wind shear, which is a change in wind speed or direction with height, is crucial for concentrating atmospheric rotation into a mesocyclone. Doppler radar is a key tool for detecting mesocyclones, allowing meteorologists to identify rotation within thunderstorms and issue tornado watches or warnings.23

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