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Propagation by the ionosphere (space wave)

For this type of propagation, electromagnetic waves are reflected by a well defined layer of the atmosphere, called the ionosphere. Ionospheric waves are used for long distance communications in the decimeter-band. The ionospheric waves, after reflection by an ionospheric layer, are once again reflected by the earth surface. Those waves follow a kind of zigzag pattern between ionospheric layer and earth surface and are able to travel over a very long distance.

During daylight, 4 different layers exist, which are reduced to two at night. Each layer has the characteristics to attenuate the radio waves and given certain circumstances, to reflect them. This is the principle used by worldwide communications.

longitude latitude nautical mile channel measure traffic

line of sight aviation terrain horizon reflection refraction sky wave ground wave

List of words

ray

phase

motion

atmosphere

initial

turbulence

temperature

beam

eddy

pressure

scattered

bouncing

humidity

layer

bending

density

troposphere

band

boundary

ionosphere

attenuate

incident

stratosphere

circumstance

transparent

height

 

index

vapor

 

dispersion

calm

 

spread

ca, circa

 

function

absorption

 

spectral width

transmission

 

droplet

carrier frequency

 

obstacle

communication

 

diffraction

conductor

 

edge

 

 

encircle

 

 

Antennas

Every radio technical system must employ an antenna to radiate and receive electromagnetic energy.

Antenna is a specialized transducer that converts incoming electromagnetic fields into alternating electric currents having the same frequencies (receiving antenna), or converts an alternating current at a specific frequency into an outgoing electromagnetic field at the same frequency (transmitting antenna). An antenna can be a simple wire or rod, or a complicated structure. Thousands of geometries and specifications are possible.

Antenna parameters

antenna gain;

antenna beam width;

radiation pattern;

aperture;

side lobes

Antenna gain

Independent of the use of a given antenna for transmitting or receiving, an important characteristic of this antenna is the gain. The ratio between the amount of energy propagated in these directions compared to the energy that would be propagated if the antenna were not directional (isotropic radiation) is known as its gain.

Some antenna sources radiate energy equally in all directions. Radiation of this type is known as isotropic radiation.

Antenna aperture (area)

The effective aperture of an antenna is the area presented to the radiated or received signal. It is a key parameter, which governs the performance of the antenna. The effective antenna aperture is measured in m2. It depends on the physical area of the antenna, the overall efficiency of the antenna (generally ranging from 50% to 80%) and the wavelength.

Radiation pattern

The radiation pattern of an antenna is a graphical depiction of the gain of the antenna (usually expressed in dB) versus angle. This will be a two-dimensional pattern, a function of both the azimuth and elevation angles.

Radiation pattern

Antenna pattern in polar

Antenna pattern in rectangular coordinates

coordinates

 

Beam width

The angular range of the antenna pattern in which at least half of the maximum power is still emitted is described as a „beam width”. The angle θ can be determined in the horizontal plane (with notation θAZ) as well as in the vertical plane (with notation θEL).

Elevation angle

The elevation angle is the angle between the horizontal plane and the line of sight, measured in the vertical plane. The elevation angle (ε) is positive above the horizon (0°elevation angle), but negative below the horizon.

is the azimuth angle; N is north direction; S is south direction; W is west direction

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