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Page Title: SKIP DISTANCE AND ZONE
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Angle of Incidence and Critical Angle
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Electronics Technician Volume 07-Antennas and Wave Propagation
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Atmospheric Effects on Propagation

SKIP DISTANCE AND ZONE Recall    from    your    previous    study    that    a transmitted  radio  wave  separates  into  two  parts, the  sky  wave  and  the  ground  wave.  With  those two   components   in   mind,   we   will   now   briefly discuss skip distance and skip zone. Skip Distance Look at the relationship between the sky wave skip    distance,    skip    zone,    and    ground    wave coverage shown in figure 1-8. The skip distance is the  distance  from  the  transmitter  to  the  point where the sky wave first returns to the earth. The skip distance depends on the wave’s frequency and angle of incidence, and the degree of ionization. Figure   1-8.—Relationship   between   skip zone, skip distance, and ground wave. Skip Zone The skip zone is a zone of  silence  between  the point  where  the  ground  wave  is  too  weak  for reception and the point where the sky wave is first returned to earth. The outer limit of the skip zone varies  considerably,  depending  on  the  operating frequency, the time of day, the season of the year, sunspot activity, and the direction of transmission. At  very-low,  low,  and  medium  frequencies,  a skip zone is never present. However, in the high- frequency spectrum,  a  skip  zone  is  often  present. As  the  operating  frequency  is  increased,  the  skip zone widens to a point where the outer limit of the skip zone  might  be  several  thousand  miles  away. At   frequencies   above   a   certain   maximum,   the outer limit of the skip zone disappears completely, and no F-layer propagation is possible. Occasionally,  the  first  sky  wave  will  return  to earth within the range of the ground wave. In this case,  severe  fading  can   result   from   the   phase difference  between  the  two  waves  (the  sky  wave has a longer path to follow). REFLECTION Reflection    occurs    when    radio    waves    are “bounced” from a flat surface. There are basically two    types    of    reflection    that    occur    in    the atmosphere:    earth    reflection    and    ionospheric reflection. Figure 1-9 shows two Figure 1-9.—Phase shift of reflected radio waves. 1-7

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