WW2010
University of Illinois

WW2010
 
  welcome
 
> online guides
 
  archives
 
  educational cd-rom
 
  current weather
 
  about ww2010
 
  index

Online Guides
 
  introduction
 
> meteorology
 
  remote sensing
 
  reading maps
 
  projects, activities

Meteorology
 
  introduction
 
  air masses, fronts
 
  clouds, precipitation
 
  el nino
 
  forces, winds
 
  hurricanes
 
  hydrologic cycle
 
> light, optics
 
  midlatitude cyclones
 
  severe storms
 
  weather forecasting

Light, Optics
 
  introduction
 
> mechanisms
 
  air, dust, haze
 
  ice crystals
 
  water droplets

mechanisms
 
  reflection
 
> scattering
 
  refraction
 
  diffraction

Scattering
 
> selective
 
  mie

User Interface
 
  graphics
> text

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Selective Scattering
better at scattering certain wavelengths than others

Scattering is a rapid process whereby light is actually absorbed by a particle and then quickly emitted in another direction.


Scattering particles can be air molecules, dust particles, water droplets or pollutants, which scatter incoming sunlight (or moonlight) in all directions, similar to how a pinball bounces around in a pinball machine. During the scattering process, no energy is lost or gained, so no temperature changes occur.

[Image: a blue sky (65K)]
Photograph by Ron L. Holle


Selective scattering occurs when certain particles are more effective at scattering a particular wavelength of light (Rayleigh scattering). Air molecules (oxygen and nitrogen, for example) are small in size, and thus more effective at scattering shorter light wavelengths (blue and violet), producing blue skies visible on a clear sunny day.

[Image: colorful sunset (50K)]
Photograph by Ron L.Holle


When the sun is low on the horizon and the atmosphere is loaded with particles, only longer wavelengths of light (yellow and red) are able to penetrate the dense atmosphere. Other wavelengths of visible light are simply scattered away and never reach our eyes, producing in a colorful sunset at the end of the day.


Terms for using data resources. CD-ROM available.
Credits and Acknowledgments for WW2010.
Department of Atmospheric Sciences (DAS) at
the University of Illinois at Urbana-Champaign.