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.
Construct an argument from evidence to explain the likelihood of an organism’s ability to survive when compared to the resources in a certain habitat (e.g., freshwater organisms survive well, less well, or not at all in saltwater; desert organisms survive well, less well, or not at all in woodlands).
Create models that illustrate how organisms and their habitats make up a system in which the parts depend on each other.