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[references/electrical/neets-modules/neets-module-10-common.htm]
SURFACE WAVES travel along the contour of the Earth by diffraction.

SPACE WAVES can travel through the air directly to the receiving
antenna or can be reflected from the surface of the Earth.

SKY WAVES, often called ionospheric waves, are radiated in an
upward direction and returned to Earth at some distant location because of refraction.
NATURAL HORIZON is the line-of-sight horizon.
Radio HORIZON is one-third farther than the natural horizon.
The IONOSPHERE consists of several layers of ions, formed by
the process called ionization.
IONIZATION is the process of knocking electrons free from their
parent atom, thus upsetting electrical neutrality.
RECombination is the opposite of ionization; that is, the free
ions combine with positive ions, causing the positive ions to return to their original
neutral atom state.
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The D LAYER is the lowest region of the ionosphere and refracts
signals of low frequencies back to Earth.
The E LAYER is present during the daylight hours; refracts signals
as high as 20 megahertz back to Earth; and is used for communications up to 1500
miles.

The F LAYER is divided into the F1 and F2 layers during the
day but combine at night to form one layer. This layer is responsible for high-frequency,
long-range transmission.
The CRITICAL Frequency is the maximum frequency that a radio
wave can be transmitted vertically and still be refracted back to Earth.

The CRITICAL ANGLE is the maximum and/or minimum angle that
a radio wave can be transmitted and still be refracted back to Earth.
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SKIP DIsTANCE is the distance between the transmitter and the
point where the sky wave first returns to Earth.
SKIP ZONE is the zone of silence between the point where the
ground wave becomes too weak for reception and the point where the sky wave is first
returned to Earth.

FADING is caused by variations in signal strength, such as absorption
of the RF energy by the ionosphere.
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MULTIPATH FADING occurs when a transmitted signal divides and
takes more than one path to a receiver and some of the signals arrive out of phase,
resulting in a weak or fading signal.

Some Transmission LOSSES that affect radio-wave propagation
are ionospheric absorption, ground reflection, and free-space losses.
ELECTROMagnetic INTERFERENCE (EMI), both natural and man-made,
interfere with radio communications.
The Maximum USABLE Frequency (MUF) is the highest frequency
that can be used for communications between two locations at a given angle of incidence
and time of day.
The LowEST USABLE Frequency (LUF) is the lowest frequency that
can be used for communications between two locations.

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OPTIMUM Working Frequency (FOT) is the most practical operating
frequency and the one that can be relied on to have the fewest problems.
PRECIPITATION ATTENUATION can be caused by rain, fog, snow,
and hail; and can affect overall communications considerably.
TEMPERATURE INVERSION causes channels, or ducts, of cool air
to form between layers of warm air, which can cause radio waves to travel far beyond
the normal line-of-sight distances.

TROPOSPHERIC PROPAGATION uses the scattering principle to achieve
beyond the line-of-sight radio communications within the troposphere.

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Answers to Questions Q1. Through Q48.
A1. Induction field and radiation field.
A2. Induction field.
A3. Radiation field.
A4. Fundamental frequency.
A5. Harmonic frequency or harmonics.
A6. 30 meters.
A7. 5 megahertz.
A8. Vertically polarized.
A9. Direction of wave propagation.
A10. Shifting in the phase relationships of the wave.
A11. Troposphere, stratosphere, and ionosphere.
A12. Stratosphere.
A13. Whether the component of the wave is travelling along the surface
or over the surface of the earth.
A14. Radio horizon is about 1/3 farther.
A15. Sea water.
A16. (a) electrical properties of the terrain (b) frequency (c) polarization
of the antenna
A17. High energy ultraviolet light waves from the sun.
A18. D, E, F1, and F2 layers.
A19. D layer is 30-55 miles, E layer 55-90 miles, and F layers are
90-240 miles.
A20. Thickness of ionized layer.
A21. Critical frequency.
A22. (a) density of ionization of the layer (b) frequency (c) angle
at which it enters the layer
A23. a zone of silence between the ground wave and sky wave where
there is no reception.
A24. Where ionization density is greatest.
A25. a term used to describe the multiple pattern a radio wave may
follow.
A26. Selective fading.
A27. Natural and man-made interference.
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A28. Natural.
A29. Man-made.
A30. (a) filtering and shielding of the transmitter (b) limiting
bandwidth (c) cutting the antenna to the correct frequency
A31. (a) physical separation of the antenna (b) limiting bandwidth
of the antenna (c) use of directional antennas
A32. Regular and irregular variations.
A33. Regular variations can be predicted but irregular variations
are unpredictable.
A34. Daily, seasonal, 11-year, and 27-days variation.
A35. Sporadic E, sudden disturbances, and ionospheric storms.
A36. MUF is maximum usable frequency. LUF is lowest usable
frequency. FOT is commonly known as optimum working frequency.
A37. MUF is highest around noon. Ultraviolet light waves from the
sun are most intense.
A38. When LUF is too low it is absorbed and is too weak for reception.
A39. Signal-to-noise ratio is low and the probability of multipath
propagation is greater.
A40. Frequent signal fading and dropouts.
A41. FOT is the most practical operating frequency that can be relied
on to avoid problems of multipath, absorbtion, and noise.
A42. They can cause attenuation by scattering.
A43. It can cause attenuation by absorbtion.
A44. It is a condition where layers of warm air are formed above
layers of cool air.
A45. It can cause VHF and UHF transmission to be propagated far beyond
normal line-of-sight distances.
A46. Troposphere.
A47. VHF and above.
A48. Near the mid-point between the transmitting and receiving antennas,
just above the radio horizon.
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