Hot air rises because it is less dense than cold air, creating an upward buoyant force. As hot air ascends, it creates a low-pressure area that draws in cooler, denser air to fill the space. This movement of air is a fundamental principle of convection, where warmer air replaces cooler air, leading to a continuous cycle of heat transfer. Ultimately, the mixing of hot and cold air helps to equalize temperatures in the environment.
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