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Saved by 2 people (0 private), first by anonymouse user on 2007-11-27


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The radiation balance of the Earth system is an accounting of the incoming and outgoing components of radiation

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radiant energy is unequally distributed over the Earth.

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Over a quarter of the available solar radiation at the top of the atmosphere is reflected or scattered back to space by particulates and clouds before it reaches the ground.

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one percent of the energy available at the top of the atmosphere is absorbed by the surface as direct and diffuse solar radiati

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direct and diffuse shortwave radiation accounts for the total incoming solar radiation or insolation (K↓).

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The proportion of light reflected from a surface is the albedo (a).

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