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Cycle
One Complete rotation through all of the values of magnitude and direction of oscillation
Frequency
The number of cycles per second. One cycle per second is called 1 Hertz
Wavelength
The physical distance between one part of a cycle and the identical part of the following cycle.
Speed of the wavelength
300,000,000 m/s
Wavelength calculations
Speed of the wave / Frequency
Frequency calculations
Speed of the wave / Wavelength
Amplitude
Maximum displacement of the oscillation away from the mean value during a cycle. (Strength of oscillation)
Phase
Amplitude of wave corresponding to an angular displacement
Phase Difference
Relationship between 2 cycles of the same frequency ("Out of Phase" = Phase difference)
Attenuation
Reduction in signal strength as distance from transmitter is increased
Types of Surfaces and there effects
Due to varying surface conductivities, a wave will travel further over sea than over dry land
Waves tend to bend towards least favourable area (bend [slow down] towards land when crossing a coast)
Modulation
The changing of frequency or amplitude by superimposing an audio frequency on a carrier frequency
Amplitude Modulation
- Frequency kept constant
- Amplitudes added to reflect modulation
Disadvantages of Amplitude Modulation
- More power required to produce AM
- For a given transmitter power, un-modulated signals will travel further than a modulated signal
- AM signals are more vulnerable to atmospheric and similar interference (static)
Frequency Modulation
- Amplitude remains constant
- Frequency is altered by superimposing modulating AND carrier waves
Advantages of Fm over Am
- Less power required
- Due to constant amplitude of transmissions, static is eliminated
Disadvantages of FM
- Radio receiver is more complex
- 'Extra' frequencies must be available to accommodate frequency modulation
Phase Modulation
: Uses the phase difference of 2 signals on the same frequency to carry intelligence.
Phase Modulation is a modulation in which the phase of the carrier wave changes according to the instantaneous amplitude of the modulating signal keeping amplitude and frequency constant
Pulse Modulation
The transmission of energy in concentrated pulses instead of a continuous wave.
Single Sideband
- Sidebands are additional frequencies
- Occur when a carrier wave is modulated by a frequency lower and higher than itself (audio frequencies)
- Carrier wave modulation consists of:
Carrier Frequency
Carrier Frequency + Audio Frequency
Carrier Frequency - Audio Frequency
- SSB = removing either 2 or 3 to reduce bandwidth usage.
3 Types of Radio Wave Propagation
- Surface Wave - Sky Wave - Direct Wave
Surface / Ground waves
- Follow earth's curvature due to:
- Diffraction and Scattering
- Caused due to obstacles redirecting radio waves downward
- Influences lower frequency waves more
Wave Tilting
- Wave contacts earth and slows down
- Responds by tilting down but energy lost = increased attenuation.
Surface/Ground Wave Restrictions, Advantages and Dis-Advantages
Restricted to VLF, LF and MF frequency ranges
Disadvantages therefore:
- Low-efficiency aerials - long aerials required
- Higher static levels
- High power demand
- High installation costs
Advantage: Long ranges of transmission possible
Sky Waves and Factors affecting Sky Waves
Caused due to refraction in ionosphere
Factors affecting Sky Waves
Frequency:
Low frequency bands become trapped or absorbed in the ionosphere
Medium/High Frequency bands are most suitable
Frequency bands >HF penetrate ionosphere and continue into space
Critical angle
The smallest angle to the vertical which is capable of producing a return wave from the ionosphere
Skip Distance
- Earth distance between the transmitter and the first returning sky wave.
- Influenced by condition of ionosphere
- Skip distance during day may be 50 miles
- As ionosphere rises during night skip distance may increase to 60 miles or more (perhaps twice)
- Signal strengths therefore vary for a given location
Dead Space
Spaces between returning Sky Waves and space from end of the Surface Wave to the next returning Sky Wave
Sky Wave Propagation within the Ionosphere
Ionised gases respond to solar radiation changes by changing density.
During the Night -
Solar radiation ceases
Ionic layers contract + density reduces
Bottom layer disappears
Ionosphere rises and influences the distance from transmitter at which a sky wave contacts Earth's surface
Factors Affecting Propagation
- Frequency in Use
- Power output of transmitter
- Obstacles in path of transmitter
Other factors affecting HF Band & GPS
- Diurnal activity/Night effect
- Seasonal activity (Annual Effects)
- 11-year sun-spot cycle
- Density of ionosphere layer
- Penetration Depth
- Critical Angle
- F layer