Convection is the transfer of heat through the movement of a fluid (such as air or water). This process occurs when a warmer, less dense fluid rises, and a cooler, denser fluid sinks, creating a continuous circulation of the fluid.
How does convection work?
Convection occurs in fluids because as the fluid is heated, its particles gain energy and move faster, causing the fluid to expand and become less dense. This less dense, warmer fluid then rises, while the cooler, denser fluid sinks. This cycle creates a convection current, which transfers heat from one place to another.
Examples of convection
Boiling water: The heat from the bottom of the pot causes the water at the bottom to become less dense and rise. As it reaches the top, it cools and becomes denser, then sinks back down to be reheated.
Atmospheric convection: The sun heats the Earth's surface, causing the air above it to warm and rise. As the warm air rises, it cools and forms clouds, eventually releasing the heat as it sinks back down.
Explore objects that can be manipulated in order to determine cause-and-effect relationships (e.g., distance between objects affecting strength of a force, orientation of magnets affecting direction of a magnetic force) of electric interactions between two objects not in contact with one another (e.g., force on hair from an electrically charged balloon, electrical forces between a charged rod and pieces of paper) or magnetic interactions between two objects not in contact with one another (e.g., force between two permanent magnets or between an electromagnet and steel paperclips, force exerted by one magnet versus the force exerted by two magnets).
Apply scientific ideas about magnets to solve a problem through an engineering design project (e.g., constructing a latch to keep a door shut, creating a device to keep two moving objects from touching each other such as a maglev system).