Geography 101 The Physical Environment
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The Radiation and Energy Balance

Radiation Balance

Radiation Balance of the Earth System

Radiation Balance Diagram
Click graphic to enlarge and learn more

(Image source: USGS http://geochange.er.usgs.gov/pub/carbon/fs97137/)


The radiation balance is the balance between incoming and outgoing components of radiant energy 

Shortwave Radiation Components

  • Direct Shortwave Radiation (S) - Shortwave radiation penetrating directly to the surface without being affected by the constituents of the atmosphere.

  • Diffuse Shortwave Radiation (D) - Shortwave radiation that has been scattered or diffused by constituents of the atmosphere (clouds, dust, etc.).

 

Scattering occurs when a beam of light is broken into several smaller, less intense beams of light by gases or particulates in the atmosphere.

 

  • Absorbed and Reflected Shortwave Radiation

    • The amount of radiation absorbed or reflected depends on the albedo of the surface.

    • Albedo is the proportion of radiation reflected from the surface, governed primarily by:

      • Surface color

      • Sun angle

albedo

Longwave Radiation Components

  • Terrestrial radiation (L (up)) - longwave radiation emitted by the earth's surface.

  • Atmospheric Counter-radiation (L (down)) - longwave radiation emitted by the atmosphere directed toward the surface

  • Amount of L (down) or L(up) depends on the temperature of the emitting body.

  • Net Radiation - is an accounting of incoming and outgoing radiation.

Q*=[(S+D)-((S+D)a)] + [L (down)- L (up)]

Energy Balance

  • Energy balance refers to how energy is used in the earth - atmospheric system

Q* = LE + H + G

 

energy balance

Energy Balance Components

Latent Energy Transfer (LE)

latent energy flux

  • LE is latent energy transfer

  • Positive LE means evaporation is taking place.

  • Negative LE means condensation is taking place.

Sensible Heat Transfer (H)

sensible heat flux

  • Positive H means that energy is used to heat up the air.

  • Negative H means the air is losing energy and cooling down.

Ground Heat Transfer (G)

ground heat flux

  • G + means that energy is transferred into the subsurface

  • G- means that energy is transferred toward the surface.

Spatial Variation of Radiation and Energy Balance Components

latitudinal net radiation

  • Sensible Heat

  • Latent Heat

Palm Beach Florida energy balance
Warm and Moist Climate

Yuma Arizona energy balance
Warm and Dry Climate

Madison WI energy balance
Cool and Humid Climate

question markCan you....

  • Explain why the sun angle varies at a place throughout the year.

  • Describe how insolation intensity varies with sun angle.

  • Describe how the earth's orbit effects seasons.

  • Describe the spatial variation of the subsolar point throughout the year.

  • Describe the three modes of heat transfer?

  • Describe the components of the radiation balance?

  • Describe the components of the energy balance and what they depend on?


 

 

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© Michael Ritter mritter@uwsp.edu
Last revised March 11, 2007