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FM 11-23.<br />

b. For radio frequencies up to about 30 mega- however, the wavelength decreases and the effect<br />

hertz (MHz), the wavelength of the transmitted of these local turbulences, which can be compared<br />

signal is large compared to the size of the turbul- to small whirlpools and bubbles in a fast moving<br />

ences encountered, and there is little effect on the stream, become increasingly important. They are<br />

transmitted signal. As the frequency is increased, the principal factors in tropo transmission.<br />

Section II.<br />

TROPO SCATTER<br />

B-4. Propagation<br />

a. Scatter Volume Turbulences. The magnitude<br />

a. As a radio wave passing through the tronumber<br />

of turbulences<br />

of the received signal depends, in part, on the<br />

poshere encounters a<br />

the transmitted<br />

turbulence,<br />

energy en-<br />

a small amount<br />

of energy is scattered away from the main<br />

counters<br />

beam<br />

in the common scatter volume. Only a<br />

of radiation. The scatter effect is the same as if small<br />

ergy<br />

portion of the resultant<br />

is directed<br />

scatter beam en-<br />

each turbulence received the signal and then rer- ergy is directed<br />

towards<br />

towards the<br />

the receiving<br />

receiving<br />

station.<br />

station.<br />

adiated it. Although the word scatter implies that<br />

aditedit.<br />

Thus, thelarger<br />

Although<br />

the scatter volume,<br />

the number<br />

the greater<br />

the spreading of the reradiated<br />

of turbulences<br />

energy<br />

encountered<br />

is<br />

and the<br />

equally<br />

probable in in all directions,<br />

directions, scattering occurs<br />

occurs<br />

more refraction of useful energy occurs. The size<br />

chiefly<br />

chiefly in<br />

in a forward<br />

forward direction<br />

direction<br />

andtherefore<br />

and, therefore<br />

the<br />

the<br />

gof the scatter volume is determined by the scatter<br />

term forward scatter is sometimes used when re- angle. As the scatter angle is increased<br />

ferring to tropo propagation. A very small portion<br />

rapidly<br />

a<br />

because<br />

moun forward t of<br />

most<br />

scatter<br />

of the<br />

ed energy<br />

of the transmitted radio wave energy reaches<br />

transmitted<br />

the<br />

energy<br />

disof the transmitted radio termincontinues wave energy reaches the<br />

out into space. Also, the amount of<br />

distant radio terminal. scattering required to return the signal to earth<br />

b. The intersection of two radio beams aimed at (receiving antenna) is increased. The distance bea<br />

common point within the troposphere forms a tween terminal stations also affects the height at<br />

common scatter volume around the intersected which the scatter volume occurs. As the circuit<br />

area (fig. B-2). The size of the scatter volume is distance is increased, the height of the scatter<br />

determined mainly by the scatter angle formed volume is also increased. Therefore, the received<br />

by the intersecting beams.<br />

signal level decreases as the circuit distance increases,<br />

if power output and other parameters re-<br />

B-5. Signal Reception<br />

main constant.<br />

The signal level received by the distance station a. Atmospheric Variations. Since tropo propais<br />

determined by several factors. Changes in any gation depends on turbulences in the atmosphere,<br />

of these factors will cause fluctuations in the changes in atmospheric conditions will affect the<br />

strength of received signals.<br />

received signal level. Daily and seasonal variations<br />

of temperature and air pressure cause longterm<br />

fading. In addition to long-term fading, the<br />

tropo signal is also characterized by very rapid<br />

fading. This rapid fading is caused by propagation<br />

over multiple paths from the scatter volume.<br />

Since the turbulent condition is constantly chang-<br />

COMMON<br />

ing, the path lengths and levels of the individual<br />

SCATTER<br />

VOLUMSTE<br />

signals are also changing. However, the composite<br />

signal level at any one time is the sum of all<br />

the signals received from each of the turbulences<br />

SCATTER ANGLE in the volume and although rapid fading may<br />

BEA M-1,, / nu / take place, no complete fadeout occurs.<br />

B-2<br />

FM 11-367-8-2<br />

Figure B-2. Geometry of tropospheric scattering.<br />

cM2 . Propagation Efficiency. A characteristic of<br />

tropo propagation is its relatively low efficiency.<br />

The scatter volume may be pictured as a very<br />

inefficient relay station, located above the horizon,<br />

receiving transmitted energy and reradiating<br />

it. Since most of the transmitted energy is not

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