It is when all bodies are at the same temperature.
When the system is in thermal equilibrium.
The transfer of heat can be considered to have ended when the temperature of the system and its surroundings have reached equilibrium, meaning they are the same. This can be determined using a thermometer or by observing that there is no further change in temperature over time.
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Convection - heat transfer through liquids.Conduction - heat transfer through solids.Radiation - heat transfer through vacuum.
We know that infrared radiation can transfer thermal energy (heat) from one place to another.
Convection heat transfer is the transfer of heat by the movement of a fluid.
For conductive and convective heat transfer, the rate of heat transfer is proportional to the the temperature difference; if you double the difference you will double the rate of heat transfer. For radiative heat transfer, the rate of heat transfer is proportional to the difference of the 4th powers of the absolute temperatures.
The convective heat transfer coefficient of water is a measure of how easily heat can move through water. A higher convective heat transfer coefficient means heat can transfer more quickly. In a system, a higher convective heat transfer coefficient can increase the rate of heat transfer, making the system more efficient at exchanging heat.
The outward transfer of Earth's internal heat helps drive mantle circulation in the Earth's interior.
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They're both modes of heat transfer via material media.
convection