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WSR-88D  SYSTEM  FUNDAMENTALS
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Aerographers Mate, Module 03-Environmental Satellites and Weather Radar
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Figure 2-26.—WSR-88D Radar Data Acquisition (RDA).

Figure 2-25.—WSR-88D system configuration. REFLECTIVITY.—Recall,    some    degree    of energy is likely to be returned to the antenna as a result of   backscattering,   and   that   size,   shape,   and composition  all  contribute  to  a  target’s  ability  to backscatter this energy. Stronger targets have higher levels of reflectivity and return more energy. Thus, stronger targets have higher reflectivity values; that is, higher  dBZ  levels.  For  example,  large  raindrops backscatter many times more power than drizzle and will produce reflectivity levels 5 to 10 dBZ higher. Because  of  its  characteristics,  hail  tends  to  have exceptionally high reflectivity values. And, since the WSR-88D  displays  information  in  the  form  of  echo intensity levels, a severe thunderstorm with hail will appear much more intense than an area of light rain or drizzle. VELOCITY.—Velocity  is  used  to  determine wind speed, direction, and target motion (perhaps the movement of a thunderstorm cell). The WSR-88D can detect small areas of convergence, divergence, and even circulation. This has proven valuable in alerting whole communities to the onset of strong surface winds and tornadic activity. SPECTRUM WIDTH.—Spectrum width data is another  method  of  determining  atmospheric  motion. Spectrum  width  examines  the  degree  of  velocity variance ofparticles (scatterers) in the atmosphere that results  from  dispersion  and  mixing.  Within  a  single sample volume of the atmosphere, many particles of varying size, shape, and composition move in different directions  and  speeds.  Because  of  their  differences, each particle moves about independently of the others. Within this single sample volume, the WSR-88D does not   sense   each   individual   motion,   but   rather   a combination  of  all  velocities  for  the  overall  sample. This  combination  of  different  velocities  is  what spectrum  width  measures. Spectrum width data is quite useful in determining atmospheric  stability,  and  is  a  good  indicator  of environmental turbulence. By itself, it offers very little guidance. Combined with other products, the user can determine radar performance and reliability of the data being displayed. The concept of evaluating spectrum width data is still relatively new and operational uses are still being developed. RDA  Subcomponents The RDA consists of all the hardware and software needed to transmit and receive radar energy. It also preprocesses raw data by filtering inconsistencies. The transmitter, receiver, and signal processor are housed together  in  a  small  building  near  the  antenna,  as 2-23

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