Propagation
5ARadio Wave Basics
5A1: Speed of Light
Radio waves are a form of electromagnetic radiation and travel at the speed of light — approximately 300,000,000 metres per second (3 × 10⁸ m/s) in free space.
- This is the fastest speed possible in the universe
- Light, radio waves, X-rays, etc. all travel at this speed
- Actual speed may vary slightly depending on the medium
5A2: Wavelength, Frequency, and Speed
Wavelength × Frequency = Speed of Light
λ × f = c
Where: λ = wavelength (metres), f = frequency (Hz), c = 3 × 10⁸ m/s
This means that as frequency increases, wavelength decreases, and vice versa.
| Frequency | Band | Approximate Wavelength |
|---|---|---|
| 3.5 MHz | 80 metres | ~80m |
| 7 MHz | 40 metres | ~40m |
| 14 MHz | 20 metres | ~20m |
| 28 MHz | 10 metres | ~10m |
| 145 MHz | 2 metres | ~2m |
| 433 MHz | 70 centimetres | ~0.7m |
5BGround Wave and Line of Sight
5B1: Ground Wave
The ground wave follows the curvature of the Earth's surface. It's useful for medium wave broadcast and LF/MF amateur bands.
- Propagates along the ground, gradually losing strength
- More effective on lower frequencies
- Affected by ground conductivity (sea water is best, dry ground is worst)
- Provides reliable local coverage
5B2: Line of Sight
On VHF and UHF frequencies, radio waves travel primarily in a line of sight — they don't follow the Earth's curve significantly.
- Range depends on antenna height and terrain
- Higher antenna = greater range
- Obstacles (hills, buildings) can block the signal
- This is why VHF/UHF repeaters are placed on high ground or tall towers
5CSky Wave
5C1: The Ionosphere
The ionosphere is a layer of the Earth's atmosphere that contains charged particles (ions) created by solar radiation. It can reflect radio waves back to Earth, enabling long-distance communication.
The ionosphere has several layers:
| Layer | Altitude | Characteristics |
|---|---|---|
| D | 60-90 km | Absorbs HF signals during the day. Disappears at night. |
| E | 90-150 km | Can reflect VHF under certain conditions (Sporadic E). |
| F1 | 150-250 km | Daytime layer. Combines with F2 at night. |
| F2 | 250-500 km | Main long-distance HF reflection layer. Highest altitude. |
5C2: Skip Distance and MUF
- Skip distance — the distance between the transmitter and the point where the reflected signal first returns to Earth
- Maximum Usable Frequency (MUF) — the highest frequency that can be reflected by the ionosphere at a given time
- Above the MUF, signals pass straight through into space
- The MUF varies with time of day, season, and solar activity
5C3: HF Propagation
Sky wave propagation is how HF radio signals travel around the world. The signal bounces between the ionosphere and the Earth's surface.
- Signals can travel thousands of kilometres by multiple "hops"
- HF propagation conditions change throughout the day
- Better propagation generally during high solar activity
- The 20m band (14 MHz) is often the most reliable for long-distance work
- Lower frequencies (80m, 40m) are better for regional contacts, especially at night
5ESporadic E
5E1: Sporadic E Propagation
Sporadic E is a propagation mode caused by small, intense patches of ionisation in the E layer of the ionosphere (90–150 km altitude). It allows VHF signals to travel much further than normal line of sight.
- Most common on VHF — particularly the 6m (50 MHz) and 2m (144 MHz) bands
- Occurs unpredictably, often in summer (May–August)
- Typically lasts minutes to hours
- Skip distances of 500–2,000 km are possible
- The E layer patches are thought to be caused by wind shear and temperature inversions
5FSolar Activity
5F1: The Solar Cycle
The Sun goes through an approximately 11-year cycle of activity. This has a major effect on HF propagation.
- Solar maximum — more sunspots, more ionisation, higher MUF, better HF propagation
- Solar minimum — fewer sunspots, lower MUF, reduced HF propagation
- Sunspots are cooler, darker areas on the Sun's surface — more sunspots = higher solar activity
5F2: Solar Effects on Propagation
Solar events can significantly affect radio propagation:
- Solar flares — sudden bursts of energy that increase D-layer absorption, causing a fade-out of HF signals (especially on lower frequencies)
- Geomagnetic storms — caused by coronal mass ejections, can disrupt the ionosphere and cause signal fading and distortion
- Increased solar activity raises the MUF, allowing higher frequencies to be used for long-distance communication
- Solar indices (SFI, A-index, K-index) are used to describe current conditions — higher SFI generally means better HF propagation