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5.2.3 Explain the enhanced greenhouse effect

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The greenhouse effect is a NATURAL PHENOMENON.
Incoming short wave radiation from the sun enters the atmosphere. Some of this is re-emitted from the earth's surface as longer wave radiation and results in heat lost to space. The rest is reflected from the earth and absorbed by greenhouse gases in the atmosphere (such as carbon dioxide, methane, oxides of nitrogen and water vapor). These then re-reflect the radiation back towards earth. This absorption of radiation by greenhouse gases results in heat being retained in the atmosphere and therefore the mean temperature of the atmosphere increases.
When the concentration of these greenhouse gases is increased, more radiation is absorbed by them and thus more heat is retained in the atmosphere. This results in a greater increase in mean temperature of the atmosphere, and this is known as the enhanced greenhouse effect.
Incoming short wave radiation from the sun enters the atmosphere. Some of this is re-emitted from the earth's surface as longer wave radiation and results in heat lost to space. The rest is reflected from the earth and absorbed by greenhouse gases in the atmosphere (such as carbon dioxide, methane, oxides of nitrogen and water vapor). These then re-reflect the radiation back towards earth. This absorption of radiation by greenhouse gases results in heat being retained in the atmosphere and therefore the mean temperature of the atmosphere increases.
When the concentration of these greenhouse gases is increased, more radiation is absorbed by them and thus more heat is retained in the atmosphere. This results in a greater increase in mean temperature of the atmosphere, and this is known as the enhanced greenhouse effect.
5.2.3 Explain the enhanced greenhouse effect
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