Page 180 - Fundamentals of Radar Signal Processing
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CHAPTER 3



                                                          Pulsed Radar Data Acquisition



               As has been seen, radar measures the spatial distribution of reflectivity in the
               three-dimensional  spherical  coordinate  system  of  range,  azimuth  angle,  and
               elevation angle. Pulsed radars do this by emitting a series of individual pulses
               and recording the received voltage as a function of time, equivalent to range.
               Modern pulsed radars use coherent receivers so that the measured voltage is
               complex valued. They also record and process the data digitally. As with any

               digital data acquisition system, the selection of sampling rates and quantization
               strategies  are  crucial  design  decisions,  affecting  signal  fidelity,  resolution,
               aliasing, and noise properties, as well as processor memory and computational
               requirements.





               3.1   Acquiring and Organizing Pulsed Radar Data


               3.1.1   One Pulse: Fast Time
               Suppose a radar transmits a single pulse of length τ seconds. The leading edge

               of the pulse is emitted at time t = 0. As discussed in Chap. 2, the echo power at
               the receiver due to clutter and targets will decay with range or time, typically at
                                            –4
                                  –1
               rates between R  and R , while the noise power generated within the receiver
               will be constant. Figure 3.1 is a notional illustration of this behavior. Depending
               on the goals of the particular radar mode of operation, the radar will measure

               the received power over some interval in range, say from R  to R . The interval
                                                                                             2
                                                                                      1
               R   – R   is  called  the range swath  or  the range window R . The range to the
                 2
                       1
                                                                                       w
               beginning of the range swath, R , may be influenced by a number of factors. For
                                                    1
               example, for an airborne downlooking radar it might equal the altitude of the
               radar,  since  no  clutter  echoes  could  occur  at  a  shorter  range.  In  a  ground
               imaging mode, it would likely be determined by the range to the nearest edge of
               the antenna mainbeam. Similarly, the end of the range swath, R , might be set in
                                                                                          2
               different  radars  by  the  far  edge  of  the  mainbeam  on  the  ground,  or  by  the

               maximum expected detection range for targets of interest. Another constraint on
               R  is the unambiguous range, to be discussed shortly.
                 2
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