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Page Title: RADIAL VELOCITY
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PHASE SHIFT
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Aerographers Mate, Module 03-Environmental Satellites and Weather Radar
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VELOCITY  ALIASING

Figure 2-19.—(A) Stationary target causing no visible change in wave characteristics, (B) Moving target displacing energy causing observable phase shifts. As another example, look at figure 2-19, view (A). Imagine  a  Doppler  radar  repeatedly  striking  a stationary target such as a building. Since the speed at which energy travels is constant, each wave returns in exactly the same phase as those before it. Now look at figure 2-19, view (B). Consider a large balloon moving slowly  toward  the  antenna.  Unlike  the  stationary building, the balloon’s motion causes a change in the appearance of each successive wave. If the radar observes these changes (phase shifts) it will realize that motion  has  occurred  and  can  then  convert  this information into target velocity. Keep in mind that the ability of a Doppler radar to detect phase shifts and compute  velocity  depends  upon  the  system maintaining a consistent transmitter frequency and phase relationship from one pulse to the next. RADIAL VELOCITY We know that Doppler radars can tell whether a target  is  moving  toward  or  away  from  the  radar. Doppler radars can also measure the velocity of the target toward or away from the antenna. Take a look at figure 2-20. At time T1 a pulse is sent towards a target and it returns at target distance "Y." At time T2, another pulse is sent towards the same target and returns a target distance of "Y+Z." The distance to the target has changed from time Tl to T2, resulting in a phase  shift  between  the  two  return  signals.  By measuring the phase shift, the wavelength, and the time interval from T1 to T2, the velocity the target moved  toward  or  away  from  the  radar  can  be computed. By convention, motion towards a Doppler radar is expressed in negative values and green (cool) colors on a display screen. Motion away from a Doppler radar is expressed in positive values and red (warm) colors. The WSR-88D’s sensitivity enables it to detect extremely  weak  reflectivities  (light  drizzle,  ice 2-18 crystals,  etc.).  This  sensitivity  allows  the  radar  to determine the wind speed from the size of the phase shift. Even dust or insects can act as scatterers and enable the WSR-88D to determine wind speeds in clear air. The  WSR-88D  will  not  always  detect  every motion in the atmosphere, nor will it display them with little or no confusion.   Since only pulsed energy that returns directly to the antenna can be detected, it stands to reason that phase shifts are only observable when they occur directly along the radar beam (radial). Figure 2-20.—Radial velocity.

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