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The radiation balance is the balance between incoming and outgoing
components of radiant energy
Shortwave Radiation Components
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Direct Shortwave Radiation
(S) - Shortwave radiation penetrating
directly to the surface without being affected by the constituents of the atmosphere.
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Diffuse Shortwave Radiation (D) - Shortwave radiation that has been
scattered or diffused by constituents of the atmosphere (clouds, dust, etc.).
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Scattering occurs when a beam of light is broken
into several smaller, less intense beams of light by gases or
particulates in the atmosphere. |
Longwave Radiation Components
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Terrestrial radiation (L (up)) - longwave radiation emitted
by the earth's surface.
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Atmospheric Counter-radiation (L (down)) - longwave radiation
emitted by the atmosphere directed toward the surface
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Amount of L (down) or L(up) depends on the temperature of the
emitting body.
Q*=[(S+D)-((S+D)a)] + [L (down)- L (up)]
Q* = LE + H + G

Energy Balance Components
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LE is latent energy transfer
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Positive LE means evaporation is taking place.
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Negative LE means condensation is taking place.
Spatial Variation of Radiation and Energy Balance Components
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Sensible Heat
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Latent Heat

Warm and Moist Climate
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Warm and Dry Climate
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Cool and Humid Climate
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Explain why the sun angle varies at a place throughout the year.
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Describe how insolation intensity varies with sun angle.
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Describe how the earth's orbit effects seasons.
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Describe the spatial variation of the subsolar point throughout the year.
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Describe the three modes of heat transfer?
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Describe the components of the radiation balance?
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Describe the components of the energy balance and what they depend on?
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