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

Remote Sensing
 
  introduction
 
  radars
 
> satellites

Satellites
 
  introduction
 
  goes satellites
 
  poes satellites
 
> image interpretation

Image Interpretation
 
  visible (vis)
 
> infrared (ir)
 
  vis -vs- ir
 
  color enhanced ir
 
  water vapor (wv)
 
  vis -vs- ir -vs- wv

User Interface
 
  graphics
> text

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Infrared Satellite Images
estimating temperature

Infrared satellite measurements are related to the brightness temperature. For an infrared picture, warmer objects appear darker than colder objects, as in the example below (a composite of data from GOES-8 and GOES-10 satellites).

[Image: example infrared satellite image (118K)]


Since temperature in the troposphere decreases with height, high level clouds are colder than low level clouds. Therefore, low clouds (like those found over North Carolina and Virginia) appear darker on an infrared image and higher clouds (like those found throughout the eastern U.S.) appear brighter. The very dark shades of gray in parts of the Rocky Mountains and in the deserts of the Southwest indicate regions where the ground is being heated by the sun.



visible (vis)
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.

vis -vs- ir