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Page Title: Seasonal Variations in the Ionosphere
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Electronics Technician Volume 07-Antennas and Wave Propagation
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Twenty-Seven Day Cycle

Table  1-1.–Daily  Ionospheric  Communications D LAYER: reflects vlf waves for long-range communications;  refracts  lf  and  mf  for short-range  communications;  has  little effect on vhf and above; gone at night. E LAYER:  depends on the angle of the sun: refracts hf waves during the day up to 20 MHz  to  distances  of  1200  miles:  greatly reduced at night. F LAYER:  structure  and  density  depend  on the time of day and the angle of the sun: consists of one layer at night and splits into two layers during daylight hours. F1 LAYER:  density depends on the angle of the sun; its main effect is to absorb hf waves passing through to the F2 layer. F2 LAYER: provides long-range hf communica- tions;   very   variable;   height   and   density change  with  time  of  day,  season,  and  sun- spot   activity. Figure  1-12.—Ionospheric layers. OTHER   PHENOMENA   THAT   AFFECT of  these  layers  is  greatest  during  the  summer.  The COMMUNICATIONS F2 layer is just the opposite. Its ionization is greatest during the winter, Therefore,   operating   frequencies Although  daily  changes  in  the  ionosphere  have for F2 layer propagation are higher in the winter than the greatest effect on communications, other phenom- ena  also  affect  communications,  both  positively  and negatively.  Those  phenomena  are  discussed  briefly in  the  following  paragraphs. SEASONAL   VARIATIONS   IN   THE IONOSPHERE Seasonal  variations  are  the  result  of  the  earth’s revolving around the sun, because the relative position of  the  sun  moves  from  one  hemisphere  to  the  other with  the  changes  in  seasons.  Seasonal  variations  of the  D,  E,  and  F1  layers  are  directly  related  to  the highest angle of the sun, meaning the ionization density in the summer. SUNSPOTS One  of  the  most  notable  occurrences  on  the  surface of the sun is the appearance and disappearance of dark, irregularly   shaped   areas   known   as   SUNSPOTS. Sunspots  are  believed  to  be  caused  by  violent  eruptions on the sun and are characterized by strong magnetic fields. These   sunspots   cause   variations   in   the ionization  level  of  the  ionosphere. Sunspots  tend  to  appear  in  two  cycles,  every  27 days  and  every  11  years. 1-10

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