Questions - Propagation
Question file 28
QUESTIONS WITH
ANSWERS STUDY NOTES
- A 'skip zone' is:
- the distance between the antenna and where the refracted wave first
returns to earth
- the distance between the far end of the ground wave and where the
refracted wave first returns to earth
- the distance between any two refracted waves
- a zone caused by lost sky waves
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- The medium which reflects high frequency radio waves back to the earth's
surface is called the:
- biosphere
- stratosphere
- ionosphere
- troposphere
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- The highest frequency that will be reflected back to the earth at any given time
is known as the:
- UHF
- MUF
- OWF
- LUF
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- All communications frequencies throughout the spectrum are affected in
varying degrees by the:
- atmospheric conditions
- ionosphere
- aurora borealis
- sun
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- Solar cycles have an average length of:
- 1 year
- 3 years
- 6 years
- 11 years
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- The 'skywave' is another name for the:
- ionospheric wave
- tropospheric wave
- ground wave
- inverted wave
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- The polarisation of an electromagnetic wave is defined by the direction of:
- the H field
- propagation
- the E field
- the receiving antenna
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- That portion of HF radiation which is directly affected by the surface of the
earth is called:
- ionospheric wave
- local field wave
- ground wave
- inverted wave
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- Radio wave energy on frequencies below 4 MHz during daylight hours is
almost completely absorbed by this ionospheric layer:
- C
- D
- E
- F
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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:
- C
- D
- E
- F
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- Scattered patches of high ionisation developed seasonally at the height of one
of the layers is called:
- sporadic-E
- patchy
- random reflectors
- trans-equatorial ionisation
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- For long distance propagation, the radiation angle of energy from the antenna
should be:
- less than 30 degrees
- more than 30 degrees but less than forty-five
- more than 45 degrees but less than ninety
- 90 degrees
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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:
- circular path going north or south from the transmitter
- great circle path
- straight line
- bent path via the ionosphere
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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:
- absorption
- baffling
- fading
- skip
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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:
- skip distance
- radiation distance
- skip angle
- skip zone
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- High Frequency long-distance propagation is most dependent on:
- ionospheric reflection
- tropospheric reflection
- ground reflection
- inverted reflection
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- The layer of the ionosphere mainly responsible for long distance
communication is:
- C
- D
- E
- F
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- The ionisation level of the ionosphere reaches its minimum:
- just after sunset
- just before sunrise
- at noon
- at midnight
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- One of the ionospheric layers splits into two parts during the day called:
- A & B
- D1 & D2
- E1 & E2
- F1 & F2
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- Signal fadeouts resulting from an 'ionospheric storm' or 'sudden ionospheric
disturbance' are usually attributed to:
- heating of the ionised layers
- over-use of the signal path
- insufficient transmitted power
- solar flare activity
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- The 80 metre band is useful for working:
- in the summer at midday during high sunspot activity
- long distance during daylight hours when absorption is not significant
- all points on the earth's surface
- up to several thousand kilometres in darkness but atmospheric and
man-made noises tend to be high
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- The skip distance of radio signals is determined by the:
- type of transmitting antenna used
- power fed to the final amplifier of the transmitter
- only the angle of radiation from the antenna
- both the height of the ionosphere and the angle of radiation from the
antenna
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- Three recognised layers of the ionosphere that affect radio propagation are:
- A, E, F
- B, D, E
- C, E, F
- D, E, F
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- Propagation on 80 metres during the summer daylight hours is limited to
relatively short distances because of
- high absorption in the D layer
- the disappearance of the E layer
- poor refraction by the F layer
- pollution in the T layer
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- The distance from the transmitter to the nearest point where the sky wave
returns to the earth is called the:
- angle of radiation
- maximum usable frequency
- skip distance
- skip zone
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- A variation in received signal strength caused by slowly changing differences
in path lengths is called:
- absorption
- fading
- fluctuation
- path loss
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- VHF and UHF bands are frequently used for satellite communication because:
- waves at these frequencies travel to and from the satellite relatively
unaffected by the ionosphere
- the Doppler frequency change caused by satellite motion is much less
than at HF
- satellites move too fast for HF waves to follow
- the Doppler effect would cause HF waves to be shifted into the VHF
and UHF bands.
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- The 'critical frequency' is defined as the:
- highest frequency to which your transmitter can be tuned
- lowest frequency which is reflected back to earth at vertical incidence
- minimum usable frequency
- highest frequency which will be reflected back to earth at vertical
incidence
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- The speed of a radio wave:
- varies indirectly to the frequency
- is the same as the speed of light
- is infinite in space
- is always less than half the speed of light
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- The MUF for a given radio path is the:
- mean of the maximum and minimum usable frequencies
- maximum usable frequency
- minimum usable frequency
- mandatory usable frequency
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- The position of the E layer in the ionosphere is:
- above the F layer
- below the F layer
- below the D layer
- sporadic
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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:
- transmitter malfunction
- selective fading
- a sudden ionospheric disturbance
- front end overload
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- Skip distance is a term associated with signals through the ionosphere. Skip
effects are due to:
- reflection and refraction from the ionosphere
- selective fading of local signals
- high gain antennas being used
- local cloud cover
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- The type of atmospheric layers which will best return signals to earth are:
- oxidised layers
- heavy cloud layers
- ionised layers
- sun spot layers
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- The ionosphere:
- is a magnetised belt around the earth
- consists of magnetised particles around the earth
- is formed from layers of ionised gases around the earth
- is a spherical belt of solar radiation around the earth
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- The skip distance of a sky wave will be greatest when the:
- ionosphere is most densely ionised
- signal given out is strongest
- angle of radiation is smallest
- polarisation is vertical
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- If the height of the reflecting layer of the ionosphere increases, the skip
distance of a high frequency transmission:
- stays the same
- decreases
- varies regularly
- becomes greater
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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:
- speed of light
- sun spot frequency
- skip distance
- maximum usable frequency
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- A 'line of sight' transmission between two stations uses mainly the:
- ionosphere
- troposphere
- sky wave
- ground wave
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- The distance travelled by ground waves in air:
- is the same for all frequencies
- is less at higher frequencies
- is more at higher frequencies
- depends on the maximum usable frequency
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- The radio wave from the transmitter to the ionosphere and back to earth is
correctly known as the:
- sky wave
- skip wave
- surface wave
- F layer
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- Reception of high frequency radio waves beyond 4000 km normally occurs by
the:
- ground wave
- skip wave
- surface wave
- sky wave
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- A 28 MHz radio signal is more likely to be heard over great distances:
- if the transmitter power is reduced
- during daylight hours
- only during the night
- at full moon
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- The number of high frequency bands open to long distance communication at
any time depends on:
- the highest frequency at which ionospheric reflection can occur
- the number of frequencies the receiver can tune
- the power being radiated by the transmitting station
- the height of the transmitting antenna
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- Regular changes in the ionosphere occur approximately every 11:
- days
- months
- years
- centuries
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- When a HF transmitted radio signal reaches a receiver, small changes in the
ionosphere can cause:
- consistently stronger signals
- a change in the ground wave signal
- variations in signal strength
- consistently weaker signals
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- The usual effect of ionospheric storms is to:
- increase the maximum usable frequency
- cause a fade-out of sky-wave signals
- produce extreme weather changes
- prevent communications by ground wave
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- Changes in received signal strength when sky wave propagation is used are
called:
- ground wave losses
- modulation losses
- fading
- sunspots
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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:
- changes in the ionosphere
- shading of the earth by clouds
- changes in atmospheric temperature
- absorption of the ground wave signal
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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:
- these waves are easily bent by the ionosphere
- these waves are easily reflected by objects in their path
- you can never tell in which direction a wave is travelling
- tall buildings have elevators
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