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Convection refers to the process of heat transfer that occurs through the movement of fluids, which can include liquids and gases. In this process, warmer portions of the fluid rise while cooler portions sink, creating a circulation pattern that distributes heat throughout the fluid. This principle is fundamental in various systems, such as heating systems, cooktops, and even atmospheric phenomena.

The significance of convection lies in its efficiency for transferring heat over distances and its role in natural processes like ocean currents or air movement. By contrast, other methods of heat transfer, such as conduction (which involves direct contact) or radiation (which involves energy transfer via electromagnetic waves), do not utilize fluid motion and are characterized by different mechanisms. Hence, the correct understanding of convection emphasizes its unique reliance on the dynamics of fluid flow for heat transfer.