From Transmitter to Receiver
From Transmitter to Receiver
Propagation
A 'skip zone' is
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The medium which reflects high frequency radio waves back to the earth's surface is called the
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The highest frequency that will be reflected back to the earth at any given time is known as the
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All communications frequencies throughout the spectrum are affected in varying degrees by the
Correct answer: sun
The sun is the primary energy source that drives radio propagation effects across the entire spectrum. Solar radiation creates and controls the ionosphere, affecting absorption, reflection, noise levels, and usable frequencies. Changes in solar activity such as the solar cycle, flares, and geomagnetic storms influence radio communications on many bands.
Solar heating also drives large-scale atmospheric behaviour, indirectly affecting refraction and attenuation at higher frequencies.
Therefore, the fundamental influence affecting communications frequencies throughout the spectrum is the sun.
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The 'skywave' is another name for the
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The polarisation of an electromagnetic wave is defined by the direction of
Correct answer: the E field
The polarisation of an electromagnetic wave is defined by the orientation of its electric field (E field) as the wave propagates through space.
For example:
Antennas are normally aligned to match the E field direction for maximum signal transfer.
Therefore, the polarisation of an electromagnetic wave is defined by the direction of the E field.
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That portion of HF radiation which is directly affected by the surface of the earth is called
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Radio wave energy on frequencies below 4 MHz during daylight hours is almost completely absorbed by this ionospheric layer
Correct answer: D layer
During daylight, the D layer becomes strongly ionised by solar radiation and causes heavy absorption of low frequency radio waves, especially below about 4 MHz. Signals at these frequencies lose most of their energy as heat in the D layer and usually do not reach higher ionospheric layers to be refracted back to Earth.
Therefore, radio wave energy below 4 MHz in daylight is almost completely absorbed by the D layer.
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Because of high absorption levels at frequencies below 4 MHz during daylight hours, only high angle signals are normally reflected back by this layer
Correct answer: E layer
During daylight, the D layer becomes strongly ionised and causes heavy absorption of radio waves below about \(4\ \mathrm{MHz}\), especially for low-angle signals. Most shallow-angle rays lose too much energy to reach higher layers.
Only high-angle (near-vertical) signals can pass through the D layer with enough remaining strength to reach the E layer, where they are refracted back to Earth, producing short-range skywave propagation.
Therefore, the layer that normally reflects only high-angle signals under these conditions is the E layer.
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Scattered patches of high ionisation developed seasonally at the height of one of the layers is called
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For long distance propagation, the radiation angle of energy from the antenna should be
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The path radio waves normally follow from a transmitting antenna to a receiving antenna at VHF and higher frequencies is a
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A radio wave may follow two or more different paths during propagation and produce slowly-changing phase differences between signals at the receiver resulting in a phenomenon called
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The distance from the far end of the ground wave to the nearest point where the sky wave returns to the earth is called the
Correct answer: skip zone
When a signal propagates by both ground wave and sky wave, the ground wave eventually weakens and dies out, while the sky wave returns to Earth some distance away from the transmitter.
The region between the end of usable ground wave coverage and the point where the sky wave first returns to Earth is called the skip zone. In this area, little or no signal is received.
Some references define skip distance as the distance from the transmitter to the first sky-wave return point. However, this question specifically describes the gap between the two coverage regions, which corresponds to the skip zone in this exam pool.
Therefore, the distance between the far end of the ground wave and the nearest sky wave return region is called the skip zone.
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High Frequency long-distance propagation is most dependent on
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The layer of the ionosphere mainly responsible for long distance communication is
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The ionisation level of the ionosphere reaches its minimum
Correct answer: just before sunrise
The ionisation of the ionosphere is caused primarily by solar radiation. During daylight, ultraviolet and X-ray energy from the sun continually creates ionisation in the ionospheric layers.
After sunset, the ionising radiation stops, but recombination (ions and electrons recombining into neutral atoms) takes time. Ionisation therefore gradually decays through the night.
The lowest ionisation level occurs just before sunrise, after the longest continuous period without solar input and before the sun begins re-ionising the atmosphere again.
Therefore, the ionisation level of the ionosphere reaches its minimum just before sunrise.
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One of the ionospheric layers splits into two parts during the day called
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Signal fadeouts resulting from an 'ionospheric storm' or 'sudden ionospheric disturbance' are usually attributed to
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The 80 metre band is useful for working
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The skip distance of radio signals is determined by the
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Three recognised layers of the ionosphere that affect radio propagation are
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Propagation on 80 metres during the summer daylight hours is limited to relatively short distances because of
The D layer is the bottom layer of the ionosphere during the daylight. It absorbs medium and high frequency waves, 10 MHz and below.
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The distance from the transmitter to the nearest point where the sky wave returns to the earth is called the
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A variation in received signal strength caused by slowly changing differences in path lengths is called
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VHF and UHF bands are frequently used for satellite communication because
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The 'critical frequency' is defined as the
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The speed of a radio wave
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The MUF for a given radio path is the
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The position of the E layer in the ionosphere is
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A distant amplitude-modulated station is heard quite loudly but the modulation is at times severely distorted. A similar local station is not affected. The probable cause of this is
Correct answer: selective fading
In amplitude modulation (AM), the signal consists of a carrier and two sidebands. During long-distance propagation, especially via the ionosphere, these components can take slightly different paths and experience different fading conditions.
When one sideband or the carrier fades more than the others, the recovered audio becomes distorted, even though the signal strength may still be strong. This effect is known as selective fading and is most noticeable on distant AM stations.
The local station is not affected because its signal arrives primarily by ground wave or short paths, so all components fade together, preserving the modulation.
Therefore, the probable cause of the distorted modulation on the distant AM station is selective fading.
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Skip distance is a term associated with signals through the ionosphere. Skip effects are due to
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The type of atmospheric layers which will best return signals to earth are
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The ionosphere
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The skip distance of a sky wave will be greatest when the
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If the height of the reflecting layer of the ionosphere increases, the skip distance of a high frequency transmission
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If the frequency of a transmitted signal is so high that we no longer receive a reflection from the ionosphere, the signal frequency is above the
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A 'line of sight' transmission between two stations uses mainly the
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The distance travelled by ground waves in air
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The radio wave from the transmitter to the ionosphere and back to earth is correctly known as the
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Reception of high frequency radio waves beyond 4000 km normally occurs by the
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A 28 MHz radio signal is more likely to be heard over great distances
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The number of high frequency bands open to long distance communication at any time depends on
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Regular changes in the ionosphere occur approximately every 11
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When a HF transmitted radio signal reaches a receiver, small changes in the ionosphere can cause
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The usual effect of ionospheric storms is to
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Changes in received signal strength when sky wave propagation is used are called
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Although high frequency signals may be received from a distant station by a sky wave at a certain time, it may not be possible to hear them an hour later. This may be due to
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VHF or UHF signals transmitted towards a tall building are often received at a more distant point in another direction because
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