January 1946 - ELECTRONICS - RADAR ON 50 CENTIMETERS - The TPS-3 Radar
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ELECTRONICS
January 1946

By Lt. Col. Harold A. Zahl
and
Major John W. Marchetti
Page 98 - 104
John Marchetti at Camp Evans
building 20 - January 1999
evans logo
These pulses are applied to the transmitter, which converts them to pulses of 600-mc energy.  They are then radiated from the antenna, which is coupled to the transmitter by means of a coaxial line.  When one of these pulses strikes an object some of the energy is reflected.  Measurement of range is facilitated by injecting into both cathode-ray tubes a series of markers spaced 107 microseconds apart, and also synchronized with the transmitted pulses.  These markers represent 10-mile intervals and provide the scale by means of which the range is measured.

Antenna and Propagation

     The antenna used with the AN/ TPS-3 is a 10-ft parabolic reflector with a radiator at its focus.  This produces a free-space beam which is about 10-deg wide at its half-power points.  Consider such an antenna situated at height h above a plane earth as shown in Fig. 5. Assume a reflecting target at point p at a great distance from the antenna.  The antenna will appear as a point source as seen from p.  The radiation pattern shows the free-space pattern of the antenna.  It is obvious that energy can reach the point p from the antenna by traveling two paths, one directly from the antenna and the second reflected from the ground.  These will be called the direct ray and the reflected ray.  The angle made by the direct ray with the horizontal is almost exactly equal to the angle made by the reflected ray and the horizontal.  Therefore, the amount of energy reaching point p along each of these two paths will be almost equal. However, because the distances along the two paths are not equal, the phase of the direct ray and the reflected ray at point p will in general not be the same. Therefore, the total energy at point p is the vector sum of the energies reaching it along the direct path and reflected path.
     In order to determine this total energy it is not necessary to know the length of each path but merely the difference between the path lengths, which will determine the difference between the phases of the direct and reflected rays at point p.  It may be assumed that the

earth is a perfect reflector. At the point of reflection there is a 180-deg change of phase. Because radio energy travels with the speed of light, 180-deg phase differences occur every half-wavelength in space. Therefore, in order for the direct ray and reflected ray to arrive in 
ELECTRONICS  -January 1946                                                                                                              101


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