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

Radars
 
introduction
 
radar basics
 
imagery
 
velocity patterns
 
applications

Radar Basics
 
radar signals
 
wave properties
 
signal scattering
 
wavelength effects
 
ray paths
 
clear air returns
 
target location
 
scanning modes
 
radial velocity

User Interface
 
graphics
text

.
Principles of Doppler Radar
for measuring target velocity

Doppler radars can measure the velocity of targets relative to the radar.

For example, at time T1 a pulse is sent towards a target and it returns a target distance "D".

2) At time T2, another pulse is sent towards the same target and returns a target distance "D + [Image: ] D".

The distance to target has changed from times T1 to T2, resulting in a phase shift between the two return signals, which Doppler radars are capable of measuring. By knowing the phase shift, the wavelength and the time interval from T1 to T2, the distance [Image: ] D that the target has moved relative to the radar can be computed. These pieces of information are then used to compute the target velocity relative to the radar. If the target is moving sideways so that its distance relative to the radar does not change, the radar will record zero velocity for that target.


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.