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
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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
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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
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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
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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
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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
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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
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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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