Physics > Communication Systems > 1.0 Elements of a communication system

  Communication Systems
    1.0 Elements of a communication system
    2.0 Radio waves
    3.0 Modulation

1.4 Earth's atmosphere
The gaseous envelope which surrounds the earth is known as earth's atmosphere.

The earth atmosphere mainly consists of nitrogen 78%, oxygen 21% along with a little portion of argon, carbon dioxide, water vapour,

hydrocarbons, sulphur compounds and dust particles.

The density of the atmospheric air goes on decreasing as we go up.

The electrical conductivity of the atmospheric air increases as we go up.

The various regions of earth's atmosphere are as follows,

  • Troposphere: It extends upto a height of 10 $km$ over earth's surface.
  • Stratosphere: It extends from 10 $km$ to 50 $km$. There is an ozone layer in stratosphere which mostly absorbs high energy radiations like ultraviolet radiations etc. coming from outer space.
  • Mesosphere: It extends from 50 $km$ to 65 $km$.
  • Ionosphere: It extends from 65 $km$ to 400 $km$.
In Ionosphere, the temperature rises to some extent with height, hence it is also known as thermosphere.

The ionosphere which is composed of ionised matter (i.e. electron and positive ions) plays an important role in space communication.

The ionosphere is subdivided into four main layers as $D$, $E$, $F_1$ and $F_2$ as shown in the table.

S.No.Name of the layerApproximate height over earth's surfaceExists duringFrequencies most affected
1$D$65 - 75 $km$Day onlyReflects LF, absorbs MF and HF to some degree
2$E$100 $km$Day onlyHelps surface waves, reflects HF
3$F_1$170 - 190 $km$Day time merges with $F_2$ at nightPartially absorbs HF waves yet allowing them to reach $F_2$
4$F_2$
300 $km$ at night,
250 - 400 $km$ during day time
Day and nightEfficiently reflects HF waves, particularly at night

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