15.07.2013 Views

Handbook of Propagation Effects for Vehicular and ... - Courses

Handbook of Propagation Effects for Vehicular and ... - Courses

Handbook of Propagation Effects for Vehicular and ... - Courses

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

Theoretical Modeling Considerations 11-3<br />

path traveled. In addition, the individual contributions undergo a Doppler shift<br />

proportional to the relative speed between any particular scatterer <strong>and</strong> the vehicle. It is<br />

limited to a b<strong>and</strong> <strong>of</strong> frequencies relative to the zero speed center frequency given by<br />

v<br />

Δ f D = ±<br />

(11-1)<br />

λ<br />

where v is the vehicle speed in m/s <strong>and</strong> λ is the wavelength in m. The positive sign<br />

denotes an increase in frequency that occurs when the vehicle moves towards the<br />

illuminated obstacle. The negative sign corresponds to a decrease in frequency occurring<br />

when the vehicle moves away from the illuminated object. This, <strong>of</strong> course, represents a<br />

worst case scenario that may occur at locations where there are sharp bends in the road.<br />

As an example, a vehicle traveling at 25 m/s ( ≈ 55 mph) receiving L-B<strong>and</strong> (1.5 GHz or<br />

λ = 0.2 m), will experience Doppler shifts limited to ± 125 Hz.<br />

11.2.2 Faraday Rotation<br />

Faraday rotation effects [Davies, 1990; Flock, 1987] are potential contributors to signal<br />

strength variations which can be neglected <strong>for</strong> LMSS systems which employ circular<br />

polarization <strong>and</strong> L-B<strong>and</strong> or above frequencies. The ionosphere contains free electrons in<br />

the relatively static Earth’s magnetic field. This combination causes polarization rotation<br />

<strong>of</strong> linearly polarized waves as given by (<strong>for</strong> f > 100 MHz)<br />

6 Be ⋅TEC<br />

φ = 1. 35 ⋅10<br />

( ° ) , 2<br />

(11-2)<br />

f<br />

where f is the frequency in Hz <strong>and</strong> Be is the effective earth's magnetic field in Webers/m 2<br />

assumed constant as a simplifying assumption <strong>and</strong> defined by<br />

B = B cosθ<br />

, (11-3)<br />

e<br />

B<br />

where B is the true Earth’s magnetic flux density at a location in the ionosphere along the<br />

Earth-satellite path <strong>and</strong> θ B is the angle between the direction <strong>of</strong> propagation <strong>and</strong> the<br />

earth's magnetic flux density vector. TEC is the total electron content (number <strong>of</strong><br />

electrons/m 2 ) given by<br />

∫<br />

3<br />

TEC = N dl ( number <strong>of</strong> electrons / m ) , (11-4)<br />

where l is the path length through the ionosphere <strong>and</strong> N (number <strong>of</strong> electrons/m 3 ) is the<br />

electron density along the path. Assuming extreme values <strong>of</strong> TEC <strong>and</strong> Be given by [ITU-<br />

R, 1986b (Report 263-6)] <strong>and</strong> <strong>for</strong> an angle <strong>of</strong> transversal <strong>of</strong> 30°<br />

18<br />

TEC = 1. 86 ⋅10<br />

(number/m 2 ), (11-5)

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!