Think about your answer, then reveal below.
Model answer: Warm air molecules move faster and spread apart, making warm air less dense. This lighter air rises, leaving fewer air molecules near the surface — which means less pressure pushing down (low pressure). Cool air molecules move slower and pack closer together, making cool air denser. This heavier air sinks, creating more molecules near the surface pushing down (high pressure).
This density difference is the engine of atmospheric circulation. Uneven heating of Earth's surface by the Sun creates warm and cool areas, which create pressure differences, which create wind. This convection process drives weather patterns from sea breezes to global wind systems.