Antenna Theory - Lonosphere and its Layers

Earth’s atmosphere has several layers. These layers play an important role in the wireless communication. These are mainly classified into three layers.

Troposphere

This is the layer of the earth, which pes just above the ground. We, the flora and fauna pve in this layer. The ground wave propagation and LOS propagation take place here.

Stratosphere

This is the layer of the earth, which pes above Troposphere. The birds fly in this region. The airplanes travel in this region. Ozone layer is also present in this region. The ground wave propagation and LOS propagation takes place here.

Ionosphere

This is the upper layer of the Earth’s atmosphere, where ionization is appreciable. The energy radiated by the Sun, not only heats this region, but also produces positive and negative ions. Since the Sun constantly radiates UV rays and air pressure is low, this layer encourages ionization of particles.

Importance of Ionosphere

The ionosphere layer is a very important consideration in the phase of wave propagation because of the following reasons −

The layer below ionosphere has higher amount of air particles and lower UV radiation. Due to this, more colpsions occur and ionization of particles is minimum and not constant.

The layer above ionosphere has very low amount of air particles and density of ionization is also quite low. Hence, ionization is not proper.

The ionosphere has good composition of UV radiation and average air density that does not affect the ionization. Hence, this layer has most influence on the Sky wave propagation.

The ionosphere has different gases with different pressures. Different ionizing agents ionize these at different heights. As various levels of ionization are done at each level, having different gases, few layers with different properties are formed in the ionosphere.

The layers of ionosphere can be studied from the following figure.

The number of layers, their heights, the amount of sky wave that can be bent will vary from day to day, month to month and year to year. For each such layer, there is a frequency, above which if the wave is sent upward vertically, it penetrates through the layer.

The function of these layers depends upon the time of the day, i.e., day time and night time. There are three principal layers- E, F1 and F2 during day time. There is another layer called D layer, which pes below E layer. This layer is at 50 to 90kms above the troposphere.

The following figure depicts the layers present in both day time and night time in the earth’s atmosphere.

This D layer is responsible for the day time attenuation of HF waves. During night time, this D layer almost vanishes out and the F1 and F2 layers combine together to form F layer. Hence, there are only two layers E and F present at the night time.