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Radar System Engineering

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88 PROPERTIES OF R.41~.l R T.-lRGE~,~ [SEC. 311<br />

denoting it by a function F(o). The aspect function F(e) {vill thus<br />

include three effects: (1) the amount of power intercepted by the area .4<br />

will depend upon the orientation of the surface with respect to the<br />

incident wave; (2) only apart of the incident radiation will be reradiated<br />

diffusely, the rest being absorbed (or, as in the case of sea return, reflected<br />

specularly); (3) the scattered power may be reradiated preferentially<br />

in certain directions, depending on the properties of the scatterers. If<br />

we let F(6) include these three factors, the expression for the effective<br />

cross section of an extended surface target becomes<br />

u = (fik) . (+CTsec 0) F(6), (31)<br />

Substitution of Eq. (31) into Eq. (30) will give the received signal S.<br />

At medium and long ranges (compared to the altitude of the airplane),<br />

the factor sec 8 is approximately unity and can be neglected. On the<br />

other hand, for the computation of the altitude signal,l Eq. (31) is not<br />

sufficiently precise, because the aspect angle o varies considerably over<br />

the large area, directly below the airplane, which lies within the range<br />

interval AR when R is approximately equal to h, the altitude. In that<br />

case, the received signal must be obtained from an integration ovrr the<br />

large area contributing to the instantaneous pow-er level in the radar<br />

receiver. z<br />

GROUND-PAINTING BY AIRBORNE RADAR<br />

BY C. F. J. OVERH.~GE.w~ R. E, CI..\PP<br />

Airborne radar equipment has been extmsively used in military<br />

aircraft for navigation by pilotage under conditions of restricted visibility.<br />

The performance of these radar sets in displaying topographic<br />

features below the aircraft depends on point-to-point variations in the<br />

radar-reflection properties of the earth’s surface. The information<br />

contained in the received echo signals is generally presented to the<br />

observer as a brightness pattern on an intensity-modulated persistentscreen<br />

cathode-ray tube in which radial distance from the center corresponds<br />

to slant range or ground range, and azimuth to relative or true<br />

bearing. While the coordinates of this plan-position indicator (PPI)<br />

presentation thus lend themselves tocornparison withmaps, the correlation<br />

between the brightness pattern and the topographic features of<br />

the ground is a matter of varying difficulty, depending on the nature<br />

of the terrain, the experience and skill of the operator, ancl the particular<br />

1The first signalto arrive is the reflectionfrom tllr ground directly I]elleaththe<br />

aircraft; it is called the “altitu(ie signal” ljcctlll>(,itsr:illge isc,cltl:ll[otlle altitudeof<br />

the aircraft.<br />

ZSee the chapter on “The .MtitudeSignal,)’ R. E. (’IJPP, “.i Theoretical and<br />

ExperiIllentalStudy of Radt~rGrotlr){iRet[lrll.'' RI, Ileport So. 1024,lYW

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