During the day, air flow is primarily influenced by the heating of the Earth's surface by the sun. As the ground warms, it heats the air above it, causing the air to rise due to decreased density. This upward movement creates a low-pressure area, drawing in cooler air from surrounding areas, which leads to a daytime breeze. This process can create local winds, such as sea breezes near coastal areas, where cooler air from the sea moves in to replace the rising warm air over land.
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