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Chapter 3

Chapter 3. Mobile Radio Propagation. Radio Frequency Bands. Types of Waves. Ionosphere ( 80 - 720 km). Sky wave. Mesosphere ( 50 - 80 km). Stratosphere ( 12 - 50 km). Space wave. Ground wave. Troposphere ( 0 - 12 km). Transmitter. Receiver. Earth . Ground Wave Propagation (LF/MF).

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Chapter 3

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  1. Chapter 3 Mobile Radio Propagation

  2. Radio Frequency Bands

  3. Types of Waves Ionosphere (80 - 720 km) Sky wave Mesosphere (50 - 80 km) Stratosphere (12 - 50 km) Space wave Ground wave Troposphere (0 - 12 km) Transmitter Receiver Earth

  4. Ground Wave Propagation (LF/MF)

  5. Sky Wave Propagation (HF)

  6. Line-of-Sight Propagation (VHF and above)

  7. Propagation Mechanisms • Reflection • Propagation wave impinges on an object which is large as compared to wavelength - e.g., the surface of the Earth, buildings, walls, etc. • Diffraction • Radio path between transmitter and receiver obstructed by surface with sharp irregular edges • Waves bend around the obstacle, even when LOS (line of sight) does not exist • Scattering • Objects smaller than the wavelength of the propagation wave - e.g. foliage, street signs, lamp posts

  8. Radio Propagation Effects Building Direct Signal Reflected Signal hb Diffracted Signal hm d Transmitter Receiver

  9. Free-space Propagation hb • The received signal power at distance d: where Pt is transmitting power, Ae is effective area, and Gt is the transmitting antenna gain. Assuming that the radiated power is uniformly distributed over the surface of the sphere. hm Distance d Transmitter Receiver

  10. Land Propagation • The received signal power: where Gr is the receiver antenna gain, L is the propagation loss in the channel, i.e., L = LP LS LF Fast fading Slow fading Path loss

  11. Path Loss (Free-space) • Path Loss: The signal strength decays exponentially with distance d between transmitter and receiver; The loss could be proportional to somewhere between d2 and d4 depending on the environment. • Definition of path loss LP : Path Loss in Free-space: where fc is the carrier frequency. This shows greater the fc , more is the loss.

  12. Path Loss (Land Propagation) • Simplest Formula: Lp = A dα where A and α: propagation constants d : distance between transmitter and receiver α : value of 3 ~ 4 in typical urban area

  13. Path Loss • Path loss in decreasing order: • Urban area (large city) • Urban area (medium and small city) • Suburban area • Open area

  14. Fading Fast Fading (Short-term fading) Slow Fading (Long-term fading) Signal Strength (dB) Path Loss Distance

  15. Slow Fading • Slow fading is caused by movement over distances large enough to produce gross variations in the overall path between transmitter and receiver. • The long-term variation in the mean level is known as slow fading (shadowing or log-normal fading). This fading caused by shadowing.

  16. Shadowing • Shadowing: Often there are millions of tiny obstructions in the channel, such as water droplets if it is raining or the individual leaves of trees. Because it is too cumbersome to take into account all the obstructions in the channel, these effects are typically lumped together into a random power loss. • Log-normal distribution: - The pdf of the received signal level is given in decibels by where M is the true received signal level m in decibels, i.e., 10log10m, M is the area average signal level, i.e., the mean of M,  is the standard deviation in decibels

  17. Fast Fading • The signal from the transmitter may be reflected from objects such as hills, buildings, or vehicles. Fast fading is due to scattering of the signal by object near transmitter. • When MS far from BS, the envelope distribution of received signal is Rayleigh distribution. The pdf is where  is the standard deviation. • Middle value rm of envelope signal within sample range to be satisfied by • We have rm = 1.777

  18. Fast Fading (Continued) • When MS far from BS, the envelope distribution of received signal is Rician distribution. The pdf is where  is the standard deviation, I0(x) is the zero-order Bessel function of the first kind,  is the amplitude of the direct signal

  19. Doppler Shift • Doppler Effect: When a wave source and a receiver are moving towards each other, the frequency of the received signal will not be the same as the source. • When they are moving toward each other, the frequency of the received signal is higher than the source. • When they are opposing each other, the frequency decreases. Thus, the frequency of the received signal is where fC is the frequency of source carrier, fD is the Doppler frequency. • Doppler Shift in frequency: where v is the moving speed,  is the wavelength of carrier.  Moving speed v MS Signal

  20. Delay Spread • When a signal propagates from a transmitter to a receiver, signal suffers one or more reflections. • This forces signal to follow different paths. • Each path has different path length, so the time of arrival for each path is different. • This effect which spreads out the signal is called “Delay Spread”.

  21. Delay Spread The signals from close by reflectors The signals from intermediate reflectors Signal Strength The signals from far away reflectors Delay

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