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Advection (By Rituraj, Garhwa, Jharkhand)
Horizontal heat transfer within the atmosphere is called advection. It refers to the movement of air masses carrying heat horizontally from one location to another.
The three types of heat transfer in the atmosphere are conduction, convection, and radiation. Conduction is the transfer of heat through direct contact, convection is the transfer of heat through the movement of fluid (air), and radiation is the transfer of heat through electromagnetic waves.
The three divisions of heat as it enters the Earth's atmosphere are conduction, convection, and radiation. Conduction is the transfer of heat through a material, convection is the transfer of heat through fluid movement, and radiation is the transfer of heat through electromagnetic waves.
Heat is transferred in the atmosphere through conduction, which is the transfer of heat through direct contact between molecules; convection, which is the transfer of heat through the movement of air or water currents; and radiation, which is the transfer of heat through electromagnetic waves, such as sunlight warming the Earth's surface.
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Conduction: Heat transfer through direct contact. Convection: Heat transfer through fluid motion, like air or water currents. Radiation: Heat transfer through electromagnetic waves. Advection: Heat transfer horizontally through the movement of air or water. Latent heat: Heat required or released during a phase change (e.g., melting, boiling). Sensible heat: Heat that causes a change in temperature of a substance without a phase change.
The transfer of heat by the movement of air currents in Earth's atmosphere is an example of convection. As warmer air rises and cooler air sinks, heat is transferred through the circulation of air in the atmosphere.
In the atmosphere, heat transfer mainly occurs through convection, as warmer air rises and cooler air sinks. In the ocean, heat transfer also primarily happens through convection currents, where warmer water rises and cooler water sinks. In Earth's interior, heat transfer occurs primarily through conduction, as heat moves from the core to the mantle and crust.
Conduction is the transfer of heat through direct contact between molecules. In the Earth's atmosphere, conduction occurs as the Earth's surface heats up the air molecules in contact with it. Convection is the transfer of heat through the movement of liquids or gases. In the Earth's atmosphere, convection currents are created as warm air rises and cool air sinks, leading to the transfer of heat. Radiation is the transfer of heat through electromagnetic waves. The Sun radiates heat through space and warms the Earth's surface and atmosphere when the electromagnetic waves are absorbed.
convection
This type of heat transfer is called radiation.