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62. Orbital Maneuvering Vehicle, NASA George C. Marshall Space Flight Center, Re- quest for Proposal l-6-pp-01438, November 1985.
 
DOWNGEOMETRYOFSKYWAVEILLUMINATIONRESULTSINSTRONGCLUTTERRETURNS INTHESAMERANGECELLASTHETARGET DEMANDINGAHIGHDYNAMICRANGEABLETOSUPPORTCLUTTER
TheReceiver.—The receiver isconventional, with ani-fbandwidth of1.8Me/see and anover-all gain ofslightly more than 120db. Instan- FIG.15.7.—Duplexing assembly. Two such units are included, one for upper-beam system and one for lower-beam system.
FREQUENCYˆAGREATADVANTAGEWHENTHERADARISMOVING SUCHASFOR3!2ˆAND THEHARDWAREISRELATIVELYINEXPENSIVEANDMATURE,&-HASBEENSUCCESSFULLYEMPLOYEDOPERATIONALLY EG INTHE53.AVY!.!03
Further trials were undertaken by ASWDU in 1945 [ 18] of an ‘improved ’discriminator, assessed in ASV Mk. VI and VIA in three Wellington Mk. XIV aircraft, with rada rs having sea return discriminators modi fied by TRE.
Lee, Y. W., and J. B.
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80 HOW RADAR WORKS discharge, or, graphically, [\/\_; and not | /|, as in the previous circuits described. This circuit acts on the principle of the ‘squegging’ oscillator, but it is important to note that the sweep frequency is not directly related to the frequency of the oscillations set up in the circuit, e HLT. ate R Swe Volt ace Synch.
Geosci. Remote Sens. 2010 ,48, 770–780.
The mainlobe of the compressed pulse at the output of the matched filter has time, or range, sidelobes that occur within time intervals of duration T, before and after the peak of the peak of the compressed pulse. The time sidelobes can conceal targets, which would otherwise be resolved using a narrow uncoded pulse. In some cases, such as phase-coded waveforms or nonlinear frequency modulation waveforms, matched filter processing alone achieves acceptable time sidelobe levels.
For example, a C-band phase shifter, operating over an 8 percent bandwidth was capable of handling 100 kW of peak power at an average power of 600 W. The insertion loss was 0.9 dB with a maximum VSWR of 1.25. However, it required 125 /rs to switch the phase.
(Prior knowledge ofthecharacteristics ofthetrajectory canbeincorporated inthemodel,as,for example, whenthetrajectory isknowntobeballistic.)Ifthedifference between theprediction andthemeasurement iszero,noadjustment ismadeandtheantenna mountispointed according tothestoredprediction. Iftheydonotagree,thetargettrajectory prediction is changed untiltheydo.Thus,thepointing oftheantenna ismadeopen-loop basedonthe storedtarget-trajectory prediction updated bytheradarmeasurements. Theservoloopthat pointstheantenna ismaderelatively wideband (highdatarate)topermitafasttracking response againsttargetswithhighangularacceleration.
= 70 cm) at zero degrees grazing angle responds to water waves of length 35 cm. These are known as gravity waves. The effect of the large water waves is to cause a tilting of the scattering surface or the smaller water waves, as in Fig.
THE
J. H. Dunn and D.
,
The experimental data collected on the wide-area surveillance mode of an airborne radar system is selected. The experiment radar parameters are illustrated in Table 2. T able 2.
55, pp. 587-S89, April, 1967. 42.
DITIONALVACUUMTUBE ORASOLID
Orle set of data5 gives the value of o0 at short wave- lengths to be proportional to U-' 6, where U is the wind speed. 'T'hc wiriti has been assunled liere to be a driving force in determining tlie radar back- scatter frotri tlie sea. It is itldccd, but tllc relation between the wind and the sea conditions is cotnplex: Iiencc, so will be the relation between the'wind and the radar backscatter.
36. Roherts, J. 8.
FIG. 18.23 Azimuth-tracking error for the passing-course target. (From A.
Marks, and A. ~loosfer: Coherent Optical Processing of Synthetic Aperture Radar Data, Proc. Soc.
12 by hail, 19.11 to 19.12 by rain, 19.8 to 19.11 Automatic detection, 7.1 to 7.2, 7.20 to 7.22 Automatic gain control (AGC), in monopulse tracker, 9.5, 9.10 to 9.11 Automatic Identification System (AIS) in civil marine radar, 22.23 to 22.25 in search and rescue, 22. 27 Automatic noise-level control, 6.23 to 6.24 Automatic Radar Plotting Aid (ARPA), 22.17 Automatic tracking, 7.22 to 7.46 alpha-beta (/g302-/g533) filter, 7.26 to 7.27, 7.30 detection acceptance, 7.25 to 7.26 I nteracting Multiple Model (IMM), 7.35 to 7.37 Kalman filter, 7.28 to 7.35 new track formation, 7.41 to 7.46 retrospective processing, 7.42 to 7.43 scheduling and control, 7.46 track association, 7.38 to 7.41 track file, 7.23 to 7.25 updating tracks, 7.26 to 7.30 AWACS, 13.65 B B-2 low cross section aircraft, 14.18, 14.42 Ballistic missile defense, 13.54 Bandwidth importance of, 1.8 to 1.9 of phased arrays, 13. 38 to 13.45 receiver, 6.9 Bar, in airborne radar, 5.15 to 5.16 Barker codes, 8.17.
This figure of merit is more representative of a " searchlighting " radar and not a surveillance radar. Ground-wave OTH radar. The type of OTH radar described in the above that propagates vra refraction from the ionosphere is sometimes called a sky-wave radar.
WARNING!%7 RADARSWEREDEVELOPEDBYTHE53.AVYTODETECTLOW
vol. IT- I. pp.
Mattern: Receivers, chap. 5 of "Radar Handbook," M. I.
Cf~andler, R. A,. and L.
28. J. C.
Its chief limitation is that the target must be in the presence of relatively large clutter signals if moving-target detection is to take place. Clutter echoes may not always be present over the range at which detection is desired. The clutter serves the same function as does the reference signal in the coherent MTI.
Further laboratory70 and theoreti - cal71 studies have shown that the major scattering feature under these conditions is the vertical stalk that emerges shortly after drop impact. Moreover, these studies suggest that the V-polarized returns from raindrop splashes should be only mildly sensitive to the rain rate, while the H-polarized returns should show a strong dependence on both the rain rate and the drop-size distribution. Something of this behavior may be seen in the data in Figure 15.17.
#/5.4%2-%!352%3 Ó{°{™ FORMATIONINORDERTOREDUCETHESPECKLENOISE4RADITIONALDIGITALMULTILOOKPROCESSING CONSISTSOFANINCOHERENTADDITIONOFINDEPENDENTIMAGESLOOKS OFTHESAMESCENE4HELOOKSCANBEOBTAINEDBYPARTITIONINGTHEAVAILABLESIGNALBANDWIDTHRANGEANDORAZIMUTH ANDPROCESSINGEACHLOOKINDEPENDENTLY4HEFINALIMAGEISPRODUCEDBYADDINGTHELOOKSINCOHERENTLY PIXELBYPIXEL4HEDIRECTTRADE
V.: Survey of Radar Signal Processing, Naval Research Laboratory Report 81 17, Washington, D.C., June 21, 1977. 64. Hansen, V.
They will thus work with thelower beam ofthesetjust described, but notwith theupper beam since thelatter is horizontally polarized. The beacon isarranged tobetriggered bythe pulses from theradar, but itreplies onadifferent frequency, toreceive which anentirely separate beacon receiving antenna and receiver system areprovided. The beacon antenna, mounted ontop ofthelower-beam radar antenna, isshown inFig.
One of the major factors in this regard has been the introduction of digital devices for conveniently computing the Fourier transform. Digital filter banks and the FFT. A transversal filter with N outputs (N pulses and N - 1 delay lines) can be made to form a bank of N contiguous filters covering the frequency range from 0 to f,, where .fp = pulse repetition frequency.
In one example. it was shown that the fading is strongly dependent on the radar and the target heights, and that for centimeter wavelengths the fading occurs at intervals of from two to three miles. The height of the evaporation duct, from which the propagation conditions can be in­ ferred, can be readily calculated from measurements of the surface water temperature and.
3/*ISBASEDONESTIMATINGTHE JAMMERPOSITIONANDPOWERLEVELANDTHENUSING SUCHESTIMATESTOADAPTTHERADARDETECTIONTHRESHOLDONLINE u*AMMERSTATEESTIMATION7HENEVERTHERADAROPERATESINTHEPASSIVEMODE IE WITH
1514] L)I?T.4ILED L).ESIG.V OF THE A.Y”/APS-10 625 sweeps between 15and 50miles, and 20-mile marks onthebeacon sweeps. 2.Arecei~’er gain control. 3.Atilt control forthe antenna.
A typical metal space-frame radome of this type might have . RADAR ANTENNAS 267 a transmission loss of 0.5 dB and cause the antenna side!obes to increase an average of 1 dB at the 25 dB level. The boresight might be shifted less than 0.1 mrad and the antenna noise temperature might increase less than 5 K.136 Approximate formulas are available for predict­ ing the electrical eITects (gain.
DIMENSIONALCOMPONENT WHERE 6ISTHEVECTORAIRMOTIONANDISCONSTRAINEDTOBEZEROATTHE SURFACE 4HEVERTICALAIR MOTIONISCALCULATEDFROMVERTICALINTEGRATIONOFTHEMASSCONTINUITYEQUATION &IGUREILLUSTRATESANAIRMOTIONFIELDOBTAINEDBYTWODOPPLERRADAROBSERVA
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B. Mack, “Basic design principles of electromagnetic scattering measurement facilities,” Rome Air Development Center Rept. RADC-TR-81-40, March 1981.
Hetland, E.; Mus é, P .; Simons, M.; Lin, Y.; Agram, P .; DiCaprio, C. Multiscale InSAR time series (MINTS) analysis of surface deformation. J.
8.6. Each phase bit consists of two lengths of line that provide the differential phase shift, and two single-pole, double-throw switches utilizing four diodes. The hybrid-coupled phase bit, as shown in Fig.
_ I · 0.443A. 0.443A. o + -00 = sm Nicos--0~ :::::: Nd cos Oo -0.443J -0.443J (}_ -00 = sin-• ··------::::::------------Nd cos 00 Nd cos 00 .
Storing the radar picture onanimage orthicon orother storage device which can berapidly scanned electrically toproduce tele- vision signals. This method, although not well developed atthe end ofthewar, holds great future promise. Use ofadark-trace tube, or“skiatron.
We then look at the apparatus moving the spot of light, and make sure that it is causing it to move at an absolutely constant speed, so that the spot does not travel faster along one part of the apparent line than it does along another. Of course, we could never do this with a mechanical lever, for it would have inertia and would take an appreciable time to get going at the start of the line, and would need to be slowed down before the end. But our electron lever has no appreciable .
be required even with some for111 of r~~echanically stabilized mounts. Data stabilizatioli is usually used with pencil-beam tracking antennas. A computer can readily calculate the angu- lar corrections to the output data to account for platform tilt.
AES , vol. 39, pp. 110–124, January 2003.
272-273, February, 1970. 43. Skolnik, M.
Itisnotsufficient thatonlythefirststageofalow-noise receiver haveasmallnoisefigure.The succeeding stagemustalsohaveasmallnoisefigure,orelsethegainofthefirststagemustbe highenoughtoswampthenoiseofthesucceeding stage.Ifthefirstnetwork isnotanamplifier butisanetwork withloss(asinacrystalmixer),thegainG1shouldbeinterpreted asanumber lessthanunity. ThenoisefigureofNnetworks incascade maybeshowntobe F=F+F2 -I+F.].-=l+...+__.!:~_-=-~_ o 1GtG1G2 G1G2'''GN-1 Similarexpressions maybederived whenbandwidths and/orthetemperature oftheindividual networks are{f1ot thesame.) Noisetemperature. Thenoiseintroduced byanetwork mayalsobeexpressed asaneffective noisetemperature, T..,definedasthat(fictional) temperature attheinputofthenetwork which wouldaccount forthenoiseliNattheoutput.Therefore Ii.N=kTeBnGand (9.6) (9.7) Thesystemnoisetemperature I:isdefinedastheeffective noisetemperature ofthereceiver systemincluding theeffectsofantenna temperature Ta.(Itisalsosometimes calledthesystem Figure9.1Twonetworks incascade..
744 RADAR SYSTEM ENGINEERING Pillbox, 276 Pip-matching, 203 Plan-position indicator, 6,167 (See ah. PPI) Plotting board, 180°, 238 verticrd, 235 x-Y, 240 Polyrod, 278 Polyrod radiators, array of,303 Pound, R.V.,717, 724 Power, formobile radar, 585 prime, supplies forradar, 555-587 forradar, inaircraft, 555-583 frequency of,555 recommendations for, 582 attied locations, 583 forlarge systems, locally generated, 584 forshipborne systems, 586 Power frequencies, inaircraft, standard, 556 Power supply, 3-phase a-cradar, 559 forultraportable equipment, 585 vibrator, 581 PPI, 167 delayed, 169 deeign of,532-545 off-center, 168 open-center, 169 pm-time-base resolution for, 544 resolved-current, 538-545 reached time bsse, 534–538 rotating-coil, 534 stretched, 170 threAone, 553 using automatic transmitter triggering, 540 PPI displays, contraat of,54*554 resolution of,548-554 Pre-plumbing, 408 Prwwrization, ofr-flines, 283, 420 PRF, choice of,598 Prime movers, small, 586 Prime power supplies for radar (see Power, prime, supplies forradar) projector, chart, 215 Propagation, free-space, 18 ofmicrowaves, over reflecting surface, 47-53 (sss ah. Microwave propagation) PSWR (see Standing-wave ratio, power)Pulse, phaae-shifted, 697 sharp, generation of,501-503 pulse cable, 386 pulse length, choice of,596-598 pulse modulation (see Modulation, polae) pulse packet, 122 pulse power (see Magnetron, pulse power of) P@e-forming network (see Network, pulseforming) Pulse-modulated doppler system, 150-157 Pulee-to-pulse cancellation, 631 Pulse recurrence frequency (see PRF) Pulee transformers, 38L-386 Puk3er, 353-390 basic circuit, 356-36o driver circuit, 371 energy sources of,387 hard-tube, 367-373 hard-tube and linetype, comparison of,3W363 line-type, 358, 374-383 a-ccharging of,383 recharging circuit of,382 switches for, 377–381 overload protection of,364 Pulser switch, 357 forline-type pulsers, 377–381 nonlinear inductance as,381 Pulser switch tubes, high-vacuum, 368 Q Q,ofcavity, 406 Quarter-wave line (see Line, quarter- wave) Quarter-wave plate, 84 R Racons, 246 Radar, 419 comparison of,with eye, 1 C-W, 127–159 comparison with pulse radar, 123 ground, use ofbeacons with, 609 history of,13 limitations of,116-126 prime power supplies for (see Power, prime, supplies forradar) principle of,3-6.
PERIODVELOCITYRESPONSECURVES)F USINGFOURINTERPULSEPERIODSMAKESTHEFIRSTNULLTOBETOODEEP THENFIVEINTERPULSEPERIODSMAYBEUSED WITHTHESTAGGERRATIOOBTAINEDBYADDINGTHEFIRSTBLINDSPEEDTOTHENUMBER
DETECTIONFUNCTIONS SUCHASINTRAPULSEMODULATIONMEASUREMENTANDWAVEFORMCODERECONNAISSANCE 0ULSEWIDTHISANUNRELIABLESORTINGPARAMETERBECAUSEOFTHEHIGHDEGREEOFCORRUP
 8I  &)'52% 2ANKDETECTOROUTPUTOFACOMPARATOR#ISEITHERAZEROORA ONEFROM'64RUNK .
 
88-91, March, 1964. 11. Ru1e.
And there is another complication. The individual ocean wave trains are not completely independent—they interact weakly and produce evanescent nonlinear product waves that, while not freely propagating, change the geometry of the sea surface and contribute to the scattered field at second order, also via Bragg scattering. Thus, as shown first by Barrick,81 the second-order scattering kernel is made up of electromagnetic and hydrodynamic terms, Γ Γ Γ = +EM HYD.
SEC.215] ATTENUATION OFMICROWAVES 61 measured, forinstance, ingrams per cubic meter. 1The effect oflarger drops ismore complicated, depending not only upon the total mass of water perunit volume, but upon thediameter ofthedrops aswell. The absorption process itself isnolonger simple, and scattering ofenergy by the drops, which depends very strongly onthe ratio ofwavelength to drop diameter, begins toplay arole.
S/N (dB) FIG. 8.7 Angular accuracy using two-pulse estimates. Feedback Integrator.
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A typical GPR achieves a range of up to a few meters, but some special systems can penetrate up to hundreds of meters or even kilometers. A few GPR systems have been operated from aircraft and from satellites to image geological features buried beneath the Saharan deserts as well as measuring the depth of the Moon and features on Mars or comets. The range of the GPR in the ground is limited because of the absorption the signal undergoes, while it travels on its two-way path through the ground material.
The primary feed should be designed with care and can be complex to give the desired aperture amplitude distribution with low spillover losses. The transmitter feed can be separated from the receiver feed by an angle a , as shown in Figure 13.30. The phase shifters are then reset between trans - mitting and receiving so that in both cases the beam points in the same direction.
Similar results were noted for the improvement in a conventional PPI when the pulses were displayed side-by-side. In other experiments with the PPI, the integration improvement has been reported to be proportional to 1.5 dB per doubling of the number of pulses, which corresponds to n"2.50 Improvements as high as 1.8 dB per doubling were also observed, but this is less than the 2.2 to 386INTRODUCTION TORADAR SYSTEMS moreinformation thaneithertheenvelope orthezero-crossings detector. itisnotsurprising thatthesignal-to-noise.ratio fromthecoherent detector isbetterthanfromtheothertwo.The improvement inthesignal-to-noise ratiomightvaryfrom1to3dBormore,overtherangeof signal-to-noise ratiosofinterest inmostradarapplications.
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RADAP. SYSTEM ENGINEERING COPYRIGHT, 1947, BY THE J1cC,R,iW-HILL BOOKCoMP.iNY,INC. PRINTELIIXTHEUNITEDSTATESOFAMERI(..< Aulr!qhhrf?send ‘1’hishook., or pert:ihrrrqf, ?na~jno!hereprod7wd in07(vJm-TII wilhottl permission oj thepublishers.
18.27 nth-Time-Around Tracking ................................. 18.30 18.6 Special Monopulse Techniques .............................. 18.30 High-Range-Resolution Monopulse ....................
For the same reason, combining the power outputs of magnetrons has not been attractive. 5. If coded or shaped pulses are required.
Dax, “Accurate tracking of low elevation targets over the sea with a monopulse radar,” in IEE Radar Conf. Publ . 105, Radar—Present and Future , London, October 23–25, 1973, pp.
MONOSTATIC TRISTATIC POLYSTATIC REALMULTISTATIC MULTI
For exam­ ple, a linear phase error across the antenna aperture causes the beam position to tilt in angle. A quadratic, or square-law, variation in phase is equivalent to defocusing the antenna. A period it: error with fundamental period pf)., where pis measured in the same units as is the wavelength 1, will produce spurious beams displaced at angles <Pn from the origin, according to the relation sin <Pn n}../p, where n is an integer.
VEILLANCE THEYALSOHAVESOMESERIOUSLIMITATIONS$EEPNULLSINELEVATIONANDPOORLOW
D.K.•andW. W.Shrader: Interclutter Visibility inMTISystems, IEEEEASCON '69 CO/welltion Record.pr.294-297, Oct.27-29,1969,IEEEPublication 69C31-AES. 46.Barton.
vol. AES-7, pp. 160-170, January, 1971.
the element pattern, it may be prudent to space the elements such that the first null of the grating lobe, rather than the peak, occurs at 90°. With N elements this more restrictive condition is given by ' N ~ 1 x 1 (711) XN 1 + lsin B0I Equation (7.8) may again be approximated by the Fourier transform of the il- lumination across the continuous aperture: sin ir(0/X)(sin B - sin B0)E(B) = V2(I + cos B) . —— (7.12) TT(a/\)(sin B — sin B0) The Fourier-transform solutions for continuous apertures19'43 may be used to approximate patterns for practical amplitude and phase distributions as long as the element-to-element spacing is small enough to suppress grating lobes.44 Monopulse difference patterns may be approximated in the same way from the Fourier transforms of the corresponding continuous odd aperture distributions.
575–576, 1988. 131. E.
16.1 16.1 Systems Using Airborne MTI Techniques .............. 16.1 16.2 Coverage Considerations ....................................... 16.2 16.3 Platform Motion and Altitude Effects on MTI Performance ...........................................................
S. Zrnic ′, Doppler Radar and Weather Observations , 2nd Ed., Mineola, NY: Dover Publications, 2006. 24.
The usual receiver, however, has some non - linearities due to detector properties and to saturation of its amplifiers by large signals. Figure 16.13 shows a typical input-output curve for a receiver. Two equal increments in input signal ( ∆i), as shown, produce dif - ferent increments in output because of the nonlinearity of this curve.
Itsvalueat aparticular samplepointisunity,butitiszeroatallothersamplepoints.]naddition, the (sint/J)!t/Jfunction canbereadilygenerated withauniform aperture distribution. The Woodward-Levinson synthesis technique 'Consists indetermining theamplitude andphaseof theuniform aperture distribution corresponding toeachofthesamplevaluesandperforming asummation toobtaintherequired overallaperture distribution. Theaperture distribution maybefoundbysubstituting theantenna patternofEq.(7.26) intotheFourier-transform relationship givenbyEq.(7.14).Theaperture distribution becomes (7.27).
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Alternatively, analytic ray-tracing can be performed on analytic profiles fitted to RTIM databases. The most accurate predictions come from the application of sophisticated ray-tracing routines to a database of RTIM snapshots. When a radiowave propaga - tion model is combined with radar system parameters, target scattering characteristics, and HF noise distributions, the radar equation (Eq.
l.- I.--__ ---J ---J ---'27.5nmifree-space range;(6)contour o 10 20 30 40 50defining startofdiffraction region. Range,nauticalmiles (Courtesy Proc.IRE.)100+­....... PROPAGATION OF RADAR WAVES 459 represents the approximate boundary between the interference region and diffraction region.
Hence, the processing QJ D .2 0. E <l Distance Figure J.18 Plot of J.1(/)) as a function of distance. (From Sa1111ders.9 IRE Trans.) .
V. RADAR TIME-BASES VERY RADAR DEVICE WHICH DEPENDS ON TIME ee ee must have a means of pulling the CRT spot along a display path at a certain speed, so that deflection from this path resulting from received signals or other pulses can be read with relation to some fixed standard. The apparatus which moves the spot in this way is known as the time-base, or more accurately as a time- base generator.
SONICAIRFRAMETOACCEPTABLELEVELS4HATBEINGTHECASE THEYDECIDEDTOANGLEALLLEADINGANDTRAILINGEDGESATACOMMONSWEEPANGLE n4HEIRPHILOSOPHYWASTHAT IFTHEYCOULDNTSUPPRESSTHEEDGERETURNS THENEXTBESTOPTIONWOULDBETOANGLETHEMALLINTOFOURCOMMONDIRECTIONSINSPACE4HUS ALLTRAILINGEDGESINTHE"
IRE, vol. 44, pp. 755-760, June, 1956.
The Sequential Observer makes a relatively prompt decision when only noise is present. The average savings also depend upon whether detection is performed coherently or noncoherently. Assuming coherent detection (pulses integrated predetection) and Pv = 0.90 and Pra = 10-8, the Sequential Observer is able to determine, on the average, that noise alone is present with less than one-tenth the number of observations required for the Neyman­ Pearson Observer.90 In the presence of a threshold signal, the Sequential Observer requires, on the average, about one-half the number of observations of the equivalent fixed-sample observer.
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However, this increases the total amount of signal processing required. The envelope at the output of the FFT is formed with a linear ( I Q2 2+ ) or square- law ( I Q2 2+) detector. Historically, linear detectors were used to manage dynamic range in fixed-point processors.
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One such niche is com - mercial weather radar, e.g., NEXRAD and TDWR. V ery High-Gain, Long-Range Radar . For very high-gain radar applications, the cost of an ESA is typically still prohibitive, and the reflector provides an economical means of realizing such high gains.
(13.17) into (13.16) yields p -_nsP,G~_ I 12 "D6 ' -1024(ln 2)R2 l 2 K 7 (13.18) Since the particle diameter D appears as the sixth power, in any distribution of precipitation particles the small number of large drops will contribute most to the echo power. Equation (13.18) does not include the attenuation of the radar energy by precipitation, which can be significant at the higher microwave frequencies and when accurate measure­ ments are required. The two-way attenuation of the radar signal in traversing the range Rand back is exp (-2tXR), where a is the one-way attenuation coefficient.