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Radar System Engineering

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62 THE RADAR EQUATION [SEC.215<br />

per kilometer, with precipitation rate in millimeters per hour. The<br />

most extensive analysis of this sort has been carried out by J. W. and<br />

D. Ryde, upon \vhose~\,ork'thecurves of Fig. 2.17 are based. The direct<br />

measurements of attenuation and rainfall which ha~’e been made confirm<br />

these predictions satisfactorily. The chief difficulty in such experiments<br />

is connected with the measurement of the rainfall, which is homogeneous<br />

in neither time nor space.<br />

The dashed curves of Fig. 2.17 show the attenuation in fog or clouds<br />

which, as we have said, does not depend on the drop diameter. According<br />

to Ryde a certain limit of optical visibility can be, at least loosely,<br />

associated with each of the dashed curves. For the conditions to which<br />

Curve f applies, for example, the optical range is limited to about 400 ft.<br />

At a wavelength of 3 mm the radar range could be 50 to 100 times as<br />

long,<br />

It would be easy, but not very instructive, to introduce an exponential<br />

factor into the radar equation to take account of the attenuation that<br />

we have been discussing. }Ve leave this task to the reader, \rho will<br />

find no difficulty in calculating, for any given case, the reduction in range<br />

caused by a specified strength of attenuation, which is effective, of<br />

course, on both the outgoing and return path. One general observation<br />

should be made, however, which is that the effect of an exponential term<br />

in the radar equation is insignificant at very short ranges but overwhelming<br />

at very long ranges. What we mean by short and long is<br />

determined by the rate of attenuation. An entirely arbitrary criterion,<br />

\rhich will serve as well as any other for discussion, is the range for \vhich<br />

the presence of the atmospheric attenuation just doubles the normal rate<br />

of decrease of signal intensity with range. If a is the rate of attenuation<br />

in db/km, the range RO so defined is given by Ro = 8.68/a km. At<br />

shorter ranges than this the inverse-square la~v is the more important<br />

factor; at ranges greater than R, the exponential factor controls the<br />

situation and any slight improvement in range must be bought at enormous<br />

price. In other words, once attenuation takes hold, it is of little<br />

avail to struggle against it.<br />

1J. IV. Ryde and D Ryde, Report 8670 of ‘~hc ResearchLaboratory of Cxeneral<br />

Electric Company,Ltd. ‘~hisis a Britishpublication.

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