Page 366 - Fundamentals of Radar Signal Processing
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FIGURE 5.14   The Tikhonov PDF for phase.



                     Other  sources  of  limitation  due  to  radar  system  instabilities  include
               instability  in  transmitter  or  oscillator  frequencies,  transmitter  phase  drift,
               coherent oscillator locking errors, PRI jitter, pulse width jitter, and quantization
               noise.  Simple  formulas  can  be  developed  to  bound  the  achievable  clutter
               attenuation  due  to  each  of  these  error  sources,  as  well  as  some  others  not
               mentioned. Still another source is PRI stagger. When used in a range-ambiguous
               scenario, PRI stagger results in clutter from different distant ranges aliasing to

               the  same  near  ranges  on  different  PRIs,  so  that  the  clutter  becomes  less
               stationary  and  the  clutter  attenuation  is  degraded. Additional  information  and
               analysis on these and other issues is available in Shrader and Gregers-Hansen
               (2008), Nathanson (1991), and Schleher (2010).
                     External to the radar, the chief factor limiting MTI improvement factor is

               simply the width of the clutter spectrum itself. Wider spectra put more clutter
               energy outside of the MTI filter null, so that less of the clutter energy is filtered
               out. This effect is evident in Eq. (5.47) and was illustrated numerically in Table
               5.1.  The  effective  clutter  spectrum  width  can  be  increased  by  radar  system
               instabilities or by measurement geometry and dynamics. For instance, a scanning
               antenna adds some amplitude modulation due to antenna pattern weighting to the
               clutter  return.  The  power  spectrum  of  the  measured  clutter  is  then  the

               convolution in the frequency domain of the actual clutter power spectrum and
               the  squared  magnitude  of  the  Fourier  transform  of  the  amplitude  modulation
               caused  by  the  antenna  scanning.  This  convolution  increases  the  observed
               spectral width somewhat. In some cases, the clutter power spectrum may not be
               centered on zero Doppler shift. A good example is rain clutter. Moving weather
               systems will have a nonzero average Doppler representing the rate at which the

               rain cell is approaching or receding from the radar system. Unless this average
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