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The process that generates much of the precipitation in the middle latitudes is primarily associated with the mid-latitude cyclones, which are large-scale weather systems. These cyclones form when contrasting air masses meet, typically a warm, moist air mass from the tropics and a cold, dry air mass from polar regions. The collision leads to the lifting of air, cooling, and condensation, resulting in cloud formation and precipitation. Additionally, frontal systems—cold fronts and warm fronts—play a crucial role in enhancing precipitation as they move through these regions.

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2w ago

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