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Heat transfer within the atmosphere occurs via all three modes of heat transfer:Conduction - as the air contacts existing heat sources. These might be surfaces that have been heated previously viaabsorptionof solar radiation or from chemical reactions

Convection - as warm air mixes with cold air as air currents move the air around and as buoyancy effects cause warm air to rise and cooler air to sink.

Radiation - much of the air is composed of heat absorbing molecules such as water vapor. Solar radiation is absorbed by these molecules, causing them to warm up.

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