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8a. Propagation

Definitions

Diagrams

Notes

Ground wave

Low frequencies are so good for world wide communication. Why are they not used more often?

Ionosphere

Radio waves are refracted by the ionosphere

ionosphere layer Position Description
D 60km - 85km - Absorbs rather than refracts radio waves
- Absorption is inversely proportional to the frequency
E 100km - 120 km - Lowest ionised layer that can usefully be used for ionospheric propagation
- Refract (bend) radio waves during daylight hours, virtually disappears at night
- Does not normally result in vast distances of communication (100s of miles, not 1000s of miles)
F 140km - 400km

150-200 kms (F1) disappears at night
- Height varies from vary rare to non-existent
- Ionises very quickly at sunrise to reach a maximum just after midday
- decay is so slow that the ionised layer remains present all through the darkness hours
- F2 layer is most important

Sky waves

Skip distances
Frequency Noon skip (km) Midnight skip (km)
1.9 MHz 0 0
3.6 MHz 0 0
7.1 MHz 0 500
10.1 MHz 350 1000
14.1 MHz 600 1600
16.1 MHz 1200 Not possible
21.1 MHz 1300 Not possible
24.9 MHz 1600 Not possible
26.5 MHz 2000 Not possible

Fading

Fade out

Other types of Propagation

1. VHF Propagation (above 30MHz)

2. Tropospheric ducting

3. Aurora / Northern lights

4. Meteor tail

5. Moon bounce

6. Amateur satellites