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Wind moves from high-pressure regions to low-pressure regions.
Uneven heating creates temperature and pressure differences.
Warm air rises over heated mountain slopes.
Valley breeze occurs during the daytime.
Dense cool air flows downhill into valleys.
Mountain breeze occurs at night.
Afternoon heating produces valley breezes.
Hilly regions such as Shimla experience these breezes.
Rising warm air creates low pressure.
These local winds influence temperature and moisture.
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