Q.In sky wave mode of propagation, why is the frequency range of transmitting signals restricted to less than 30 MHz?
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Ground Wave and Sky Wave Propagation
Think about shouting across a field. If the ground is flat and clear, your voice carries a certain distance. But if you shout toward a cliff, the sound bounces back as an echo. Radio waves behave in a similar way — they can either hug the Earth's surface or bounce off a layer in the sky.
The two fundamental modes of long-distance radio communication are ground wave propagation and sky wave propagation. They differ entirely in how the wave travels from transmitter to receiver.
Ground Wave Propagation
Intuition: Imagine a wave that sticks to the ground like a train on tracks. It doesn't leap into the sky; it curves along the Earth's curvature, following the surface.
Precise statement: Ground wave propagation (also called surface wave propagation) is the mode in which radio waves travel along the surface of the Earth, guided by the ground. The wave's electric field induces currents in the ground, and the wave itself diffracts around the Earth's curvature.
This works best at low and medium frequencies (typically up to about 2–3 MHz). The ground acts as a partial conductor, and the wave "attaches" itself to it. Because the Earth is curved, the wave bends around it — this is diffraction, not reflection.
Ground waves are vertically polarised. A vertical antenna is used because the electric field must be perpendicular to the conducting ground for efficient propagation.
Key characteristics:
- Range: up to a few hundred kilometres (depends on transmitter power and ground conductivity)
- Attenuation increases rapidly with frequency — higher frequencies get absorbed by the ground
- Used by AM radio (530–1600 kHz) and maritime communication
Why does it fade? The ground is not a perfect conductor. Energy is continuously lost as heat in the soil or seawater. Seawater (salty) is a much better conductor than dry soil, so ground waves travel farther over the ocean.
Sky Wave Propagation
Intuition: Now think of throwing a ball at a wall. If the wall is soft and bouncy, the ball comes back. In the sky, there is a natural "wall" made of charged particles — the ionosphere. Radio waves aimed upward can bounce off this layer and come back down hundreds or thousands of kilometres away.
Precise statement: Sky wave propagation (also called ionospheric propagation) is the mode in which radio waves are reflected (or refracted) back to Earth by the ionosphere — a region of the upper atmosphere (about 60–600 km altitude) containing free electrons and ions.
The ionosphere is not a hard surface. It bends the wave gradually through refraction, not a single bounce. The wave enters the ionised layer, slows down, and bends back toward Earth when the electron density is high enough.
| Common misconception | Truth |
|----------------------|-------|
| The ionosphere reflects waves like a mirror | It refracts them gradually — the bending is continuous, not a single bounce |
| All frequencies reflect equally | Only frequencies below about 30–40 MHz reflect; higher frequencies (VHF, UHF) pass straight through |
Key characteristics:
- Works for high frequencies (HF): 3–30 MHz
- Range: thousands of kilometres (even intercontinental) via multiple hops
- Used by shortwave radio, amateur radio, and some military communications
- The ionosphere changes with time of day, season, and solar activity — so sky wave propagation is unreliable compared to ground wave …
Part (b)Concept understanding — Ground Wave and Sky Wave Propagation
Ground Wave and Sky Wave Propagation
Think about shouting across a field. If the ground is flat and clear, your voice carries a certain distance. But if you shout toward a cliff, the sound bounces back as an echo. Radio waves behave in a similar way — they can either hug the Earth's surface or bounce off a layer in the sky.
The two fundamental modes of long-distance radio communication are ground wave propagation and sky wave propagation. They differ entirely in how the wave travels from transmitter to receiver.
Ground Wave Propagation
Intuition: Imagine a wave that sticks to the ground like a train on tracks. It doesn't leap into the sky; it curves along the Earth's curvature, following the surface.
Precise statement: Ground wave propagation (also called surface wave propagation) is the mode in which radio waves travel along the surface of the Earth, guided by the ground. The wave's electric field induces currents in the ground, and the wave itself diffracts around the Earth's curvature.
This works best at low and medium frequencies (typically up to about 2–3 MHz). The ground acts as a partial conductor, and the wave "attaches" itself to it. Because the Earth is curved, the wave bends around it — this is diffraction, not reflection.
Ground waves are vertically polarised. A vertical antenna is used because the electric field must be perpendicular to the conducting ground for efficient propagation.
Key characteristics:
- Range: up to a few hundred kilometres (depends on transmitter power and ground conductivity)
- Attenuation increases rapidly with frequency — higher frequencies get absorbed by the ground
- Used by AM radio (530–1600 kHz) and maritime communication
Why does it fade? The ground is not a perfect conductor. Energy is continuously lost as heat in the soil or seawater. Seawater (salty) is a much better conductor than dry soil, so ground waves travel farther over the ocean.
Sky Wave Propagation
Intuition: Now think of throwing a ball at a wall. If the wall is soft and bouncy, the ball comes back. In the sky, there is a natural "wall" made of charged particles — the ionosphere. Radio waves aimed upward can bounce off this layer and come back down hundreds or thousands of kilometres away.
Precise statement: Sky wave propagation (also called ionospheric propagation) is the mode in which radio waves are reflected (or refracted) back to Earth by the ionosphere — a region of the upper atmosphere (about 60–600 km altitude) containing free electrons and ions.
The ionosphere is not a hard surface. It bends the wave gradually through refraction, not a single bounce. The wave enters the ionised layer, slows down, and bends back toward Earth when the electron density is high enough.
| Common misconception | Truth |
|----------------------|-------|
| The ionosphere reflects waves like a mirror | It refracts them gradually — the bending is continuous, not a single bounce |
| All frequencies reflect equally | Only frequencies below about 30–40 MHz reflect; higher frequencies (VHF, UHF) pass straight through |
Key characteristics:
- Works for high frequencies (HF): 3–30 MHz
- Range: thousands of kilometres (even intercontinental) via multiple hops
- Used by shortwave radio, amateur radio, and some military communications
- The ionosphere changes with time of day, season, and solar activity — so sky wave propagation is unreliable compared to ground wave …
Part (a)
Sky-wave communication relies on the ionosphere reflecting the signal back to Earth, which happens only while the frequency stays below the ionosphere's (angle-adjusted) plasma/critical frequency. The critical frequency of the reflecting layers is only about 10–12 MHz, and even at oblique incidence reflection fails above roughly 30 MHz — such waves penetrate the ionosphere and escape into space instead of returning. …
Part (a): above ~30 MHz radio waves penetrate the ionosphere instead of reflecting, so sky-wave propagation is restricted to below ~30 MHz.
Part (b): ground-wave range depends on transmitter power, frequency (lower travels farther), and surface conductivity.
Part (a): Why Sky-Wave Frequencies Are Below ~30 MHz
The ionosphere acts as a frequency-selective mirror. A wave of frequency f is reflected only if f is below the local plasma frequency fp=9Ne (adjusted upward for oblique incidence), where Ne is the electron density.
- The reflecting layers have critical frequencies of only about 10–12 MHz for vertical incidence.
- At oblique incidence the maximum usable frequency rises (secant law) to around 30 MHz.
- For f≳30 MHz the free electrons cannot respond fast enough; the wave passes through the ionosphere and escapes into space rather than returning to Earth. …
- CBSE 2019Set 55/1/11 markQ.In sky wave mode of propagation, why is the frequency range of transmitting signals restricted to less than 30 MHz?(OR)On what factors does the range of coverage in ground wave propagation depend?
›Reveal solutionSolution
Part (a): above ~30 MHz radio waves penetrate the ionosphere instead of reflecting, so sky-wave propagation is restricted to below ~30 MHz.
Part (b): ground-wave range depends on transmitter power, frequency (lower travels farther), and surface conductivity.
Part (a): Why Sky-Wave Frequencies Are Below ~30 MHz
The ionosphere acts as a frequency-selective mirror. A wave of frequency f is reflected only if f is below the local plasma frequency fp=9Ne (adjusted upward for oblique incidence), where Ne is the electron density.
- The reflecting layers have critical frequencies of only about 10–12 MHz for vertical incidence.
- At oblique incidence the maximum usable frequency rises (secant law) to around 30 MHz.
- For f≳30 MHz the free electrons cannot respond fast enough; the wave passes through the ionosphere and escapes into space rather than returning to Earth. …
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