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In the Midwest, storms typically rotate counterclockwise due to the Coriolis effect, especially in the case of low-pressure systems. This rotation is part of the larger atmospheric circulation patterns, where warm, moist air rises and is replaced by cooler air. Severe thunderstorms and tornadoes often form in this region, influenced by the interaction of warm, humid air from the Gulf of Mexico and cooler, drier air from Canada. The resulting storm systems can exhibit strong rotational characteristics, particularly in supercell thunderstorms.

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1mo ago

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