WW2010
University of Illinois

WW2010
 
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Online Guides
 
  introduction
 
  meteorology
 
> remote sensing
 
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Remote Sensing
 
  introduction
 
> radars
 
  satellites

Radars
 
  introduction
 
  radar basics
 
> imagery
 
  velocity patterns
 
  applications

MDR Imagery
 
> introduction
 
  tops & movement
 
  type & tendencies

User Interface
 
  graphics
> text

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MDR Radar Imagery
detecting precipitation

The word radar stands for Radio Detection and Ranging and radar images are useful for locating precipitation. As an X-ray machine examines the inside of a human body, a radar examines the inside of a cloud. A radar sends out signals into the atmosphere and if any precipitation is present, the radar signal is scattered back to the radar transmitter. These returned signals, called radar echoes, are used to produce radar images.


The location of the colored radar echoes indicate where precipitation is falling and the various colors indicate the intensity of the precipitation through the color code in the legend below.


Shades of blue represent lighter precipitation while red and purple indicate heavier precipitation. The example radar image above shows extensive precipitation from Kansas into Ohio associated with showers and thunderstorms that developed during the late afternoon hours of August 15, 1995. Regions of light and dark blue indicate regions of lighter precipitation while areas of red and purple indicate strong, to occasionally severe thunderstorms.

These radar images DO NOT specify precipitation type, as is seen with some newer products, only the location of precipitation and its intensity. Therefore, dark blue could represent either light rain or light snow, depending upon the weather conditions that existed at the time the radar image was generated.


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.