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It is simply a function computed from the reciprocal of a true adapted antenna pattern. Superresolution and adaptive antennas for jammer can - cellation are intimately related. Roughly speaking, the difference is that one produces a pattern with the nulls down (adaptive antenna for jammer cancellation) and the other with the nulls up, i.e., peaks (superresolution of jammers). |
The prime difference between optical and microwave refraction is that water vapor has a negligible effect on the former; consequently the second term of Eq. (12.9) may be neglected at optical frequencies. Since the barometric pressure p and the water-vapor content e decrease rapidly with height, while the temperature T decreases slowly with height, the index of refraction normally decreases with increasing altitude. |
MALLY BENIGN CONDITIONS ON THE BRIDGE OF A LARGE MODERN SHIP THE DISPLAY AND RADAR PROCESSOR CAN BE SUBJECT TO HIGH LEVELS OF SHOCK AND VIBRATION AND MUST MEET HIGH VARIATIONS IN TEMPERATURE |
A P-4. pp. 60, 609, October, 1956. |
ALARM PROBABILITY ACCORDING TO 0F |
The induction motor rating should beabout 50per cent larger than that required todrive the alternator. Itis desirable tohave the alternator output the same asthe ship’s power so that theradar system can beoperated directly from the ship’s supply in case ofbreakdown ormaintenance shutdown ofthemotor-alternator set. The motor may bedirect-coupled orbelt-connected tothealternator; usually direct coupling ispreferred because ofitssimplicity. |
Arancibia, “A sidelobe blanking system design and demonstration,” Microwave J ., vol. 21, pp. 69–73, March 1978; reprinted in Ref. |
.2#3 . '2/5.$ 0%.%42!4).' 2!$!2 Ó£°Ó£ THAT THE PEAK SIGNAL OUTPUT TO MEAN NOISE RATIO IS GREATER THAN CAN BE ACHIEVED WITH ANY OTHER LINEAR FILTER 4HIS IS NOT ALWAYS THE BEST FILTER TO USE FOR TIME |
(24), thegreatest possible subclutter visibility is26db. There isthen noneed tomake theindividual subclutter risibilities forscanning and wind greater than 30db. For thecase ofscanning, that means, from Eq. |
Raven, and P. Waterman, Airborne Radar , Boston: Boston Technical Publishers, 1965, pp. 203–207. |
The echo from the ground directly beneath the aircraft is called the altiwde return. The altitude return is not shifted in frequency since the relative velocity between radar and ground is essentially zero. Clutter to either side of the perpendicu lar will have a relative-velocity component and hence some doppler frequency shift; con sequently the clutter spectrum from the altitude return will be of finite width. |
Thechoiceofpolarization alsoinfluences thea'mount ofseaorlandabsorption. Vertical polarization isabsorbed morethanhorizontal. Thetotalantenna temperature canbefoundbyintegrating thetemperature" seen"bythe antenna, weighted bytheantenna gainovertheentiresphere.60 '7:~'f78(0,c/J)G(O,c/J)dO. |
Practical Detectors. Many different detectors (often called integrators ) are used to accumulate the radar returns as the radar sweeps by a target. A few of the most common detectors7 are shown in Figure 7.3. |
10.22 RADAR HANDBOOK 6x9 Handbook / Radar Handbook / Skolnik / 148547-3 / Chapter 10 rectangular pulse, a large bandwidth would likely cause interference to other radars and other electromagnetic systems. For this reason, government frequency allocation agencies usually require that the frequency spectrum from a radar not contain large energy at other frequencies. This is becoming more important as the occupancy of the electromagnetic spectrum is increasingly crowded with transmitters. |
This is especially useful in an air-traffic-control display in which such information as target ide~ltity a~id altitude is desired to be displayed. The positions of targets on a predeterniiried number of previous scans might be shown on a synthetic display, or a line might be generated tb indicate the direction of the target's trajectory and the target's speed. (The length of the line can be made proportional to target speed.) The use of a computer to generate the grapllicq arid coritrol the CRT display offers flexibility in the choice of such things as range scales, olfcenter displ;ty, blow-up of selected areas, physical map outlines, grid displays, airport runways, stored clutter map, raw video, outlines of areas of weather blanked by the operator, tlispiay of stored flight plans, arid time-compressed display of several successive radar scans. |
S. Pearson, “On the problems of the most efficient tests of statistical hypoth - eses,” Philos. Trans. |
The entire unit rotates at a 6 rpm rate. It houses a broadside array of Yagi-type endfire elements. It' 1. |
SIGHT PROPAGATION IS TO REDUCE THE ANGLE OF THE LOWEST LOBE BRINGING IT CLOSER TO THE SURFACE & $ ! #! ## ! %% "'! !$$( |
Lines ofconstant height arehorizontal and equally spaced. Arrangements aresometimes made tomove therange origin offthetube face toallow expansion ofaregion ofinterest. Iftheheight-finding antenna isrequired toscan over anappreciable range ofazimuth angles, theRHI isusu- ally blanked except during arelatively10,OOO narrow azimuth sector, inorder toimprove the ratio ofsignal tonoise and toavoid ZPconfusion between targets atdifferent ; azimuths. |
This was said to apply to a good operator viewing a PPI under good conditions. Its degree of applicability, however, is not clear. It is not iinusual to find no accoutlt of the operator loss being taken in the radar equation. |
705-706, December, 1957. 50. Payne-Scott, R.: The Visibility of Small Echoes on Radar PPI Displays, Proc. |
2 INTRODUCTION TO RADAR SYSTEMS The name radar reflects the emphasis placed by the early experimenters on a device to detect the presence of a target and measure its range. Radar is a contraction of the words radio detection and ranging. It was first developed as a detection device to warn of the approach of hostile aircraft and for directing antiaircraft weapons. |
MADE SLING OR HARNESS TO SUPPORT THE TARGET 4HE FIRST USES A SINGLE OVERHEAD SUPPORT POINT AND GUY LINES TO A FLOOR |
Tlle evaporation duct that lies just above the surface of the sea is a result of tlie water vapor. or liumidity, evaporated from the sea. The air in contact with the sea is saturated 14tIi water vapor, wit11 a saturation vapor pressure appropriate to the temperature of tl~e sea si~rface.'~ The air several meters above the sea is not usually saturated so there will be a gradual decrease in water vapor pressure from the surface value to the ambient value well above tlie surface. |
%*$) '!# ' |
Platform is a generic term referring to the vehicle where the radar and antenna are installed. Typical radar platforms include pedestal (fixed site), ground vehicles, ships, airplanes, UA Vs, and spacecraft/satellites. The following short section is devoted to platform impacts and some key associated design drivers. |
Some of the prediction methods have not been well documented although widely distributed; also, users frequently “improve” upon a model and prediction method to suit their specific needs. As an example, the model RADAR C29 is the basic building block of Thomason et al. in NRL Report 832122; however, they added a D region, a collision-frequency distribution, an Earth’s magnetic field, a topside elec - tron distribution, an auroral electron-density modification,34 and other features that make the model more generally useful. |
Conf ., September 14–16, 1964, pp. 259–263. 11. |
The term pseudo-monostatic will be used to characterize bistatic geometries that approximate monostatic operation. 23.2 COORDINATE SYSTEMS A two-dimensional north-referenced coordinate system21 is used throughout this chapter. Figure 23.1 shows the coordinate system and parameters defining bistatic radar opera - tion in the ( x, y) plane, also called the bistatic plane .22 The bistatic triangle lies in the bistatic plane. |
The sine pulse, inaddition toitstracking role, triggers aflip-flop controlling the cosine-pulse switch, and thecosine pulse similarly triggers aflip-flop con- trolling themodulator pulse switch. The modulator pulse ispassed onto theindicators and, inaddition, triggers aflip-flop which closes theswitch ahead ofthedecoder while video signals arebeing received, and opens it shortly before thenext basic pulse. Afew words should besaid about theprocess of“locking in” initially orafter tracking has been lost through failure ofsignals orsevere inter- ference. |
It was shown in Chap. 2 that the dividing line between these two regions depended upon the probability of a false alarm, which in turn is related to the average time between false alarms. There are two types of errors that might be made in the decision process. |
Electron ., vol. 16, pp. 170–185, October 1984. |
Maffett, F. Smith, R.C. Heimiller, and A. |
24,Sec. 6.2. The latter effect makes the detection ofadesired target echo within therain clutter even more difficult, forthevery persistence ofthetarget echo onsuccessive pulses helps greatly todistinguish itfrom noise (Sec. |
In fact, the sharp falloff of the nonducting data in Figure 15.18 might be further evidence of the threshold shadowing mentioned earlier. However, the common idea of shadowing derives from the geometrical optics concept of a sharp transition between light and darkness. By considering the implications of diffraction at the wave peaks, it is possible to determine the domain of radar frequen - cies and wind speeds over which the concepts of geometrical optics may be applied. |
Further, it can be shown that the average SCR improvement calculated for a single filter is equal to the MTI improvement factor as defined in Sec. 15.4. The basis for obtaining the optimum MTI filter is again the covariance matrix of the clutter returns as given by Eq. |
(Ajler Sa~nders,~ IRE Trans.) CWANDFREQUENCY-MODULATED RADAR89 whereJ0,JI,J2,etc=Besselfunctions offirstkindandorder0,I,2,etc.,respectively D=(~I/f~)sin2rrf~Role Ro=distance totargetattimet=0(distance thatwouldhavebeenmeas urediftargetwerestationary) c=velocity ofpropagation Id=2l',.f~/c=doppler frequency shift 1',=relative velocity oftargetwithrespecttoradar <Po=phaseshiftapproximately equaltoangular distance 4rrfoRole cPm=phaseshiftapproximately equalto2rrfmRole Thedifference-frequcncy signalofEq.(3.16)consists ofadoppler-frequency component ofamplitude Jo(D)andaseriesofcosinewavesoffrequency 1m'~rm,~rm'etc.Eachofthese harmonics off~ismodulatcd byadoppler-frequency component withamplitude proportional toJn(IJ).Theproduct ofthedoppler-frequency factortimesthenthharmonic factorisequiva lenttoasuppressed-carrier double-sidcband modulation (Fig.3.15). Inprinciple, anyoftheJncomponents ofthedifference-frequency signalcanbeextracted inthcFM-CW radar.Consider firstthedoctermJo(D)cos(2rrfdt-4>0)'Thisisacosinewave atthctloppler frequency withanamplitude proportional toJo(D).Figure3.16showsaplotof severaloftheBesselfunctions. Theargument DoftheBesselfunction isproportional torange. |
22.11 Maximum time for viewing objects from a space vehicle if the objects are tracked.28 3. Atmospheric propagation problems can be minimized by proper selection of operating frequencies and favorable geometry selection. 4. |
The MTI in the lower beams can be optimized for surface clutter and MTI in the upper beams, ~f used at all, can be optimized for rain and chaff. The individual pencil beams have a higher gain than a fan-beam antenna, and can provide a larger number of hits at a higher data rate than can a 3D radar with a single scanning beam in elevation. -) Scanning pencil beam. |
Any use is subject to the Terms of Use as given at the website. Electronic Counter-Countermeasures. ELECTRONIC COUNTER-COUNTERMEASURES 24.636x9 Handbook / Radar Handbook / Skolnik / 148547-3 / Chapter 24 100. B. |
11.6 Measured RCS pattern of a dipole 5.221X long. (Courtesy of University of Michigan Radiation Laboratory.6) Figure 11.7 shows the broadside resonances of a wire dipole as a function of dipole length. The first resonance occurs when the dipole is just under a half wavelength long, and its magnitude is very nearly X2. |
III and ASV Mk. VI are shown in figures 4.33 and4.34. Figure 4.33 compares detection ranges for a U class submarine, either beam-on or end-on to the radar. |
23-25, 1973, pp. 292-296. 42. |
MTI-14, pp. 24 -28, January, 1966. 41. |
STAP is a fairly broad topic that has applicability beyond this chapter on airborne MTI radar. The primary motivation for STAP is to improve clutter cancellation perfor - mance and to better integrate a radar’s spatial processing (antenna sidelobe control and sidelobe jamming cancellation) with its temporal clutter cancellation processing. The applicability of STAP to improving clutter cancellation must be assessed spe - cifically in the context of the key performance limiters to airborne MTI radar clut - ter cancellation as described at the start of this chapter. |
11.20. This device generates a binary pseudorandom code of zeros and ones oflength 2" I, where n is the number of stages in the shift register. Feedback is provided by taking the output of the shift register and adding it, modulo two, to the output from one of the previous stages of the shift register. |
POLARIZED RETURNS FROM VOLUME SCATTERERS WITH ELEMENTS THAT ARE LARGE COMPARED WITH A WAVELENGTH ARE STRON |
A single "snapshot" of a PPI would not likely differentiate the echo of a small target from that of the sea spikes. The individual sea spikes, however, will disappear with time and new spikes will appear at other locations. If it is possible to observe the radar display for a sufficient period of time, the small targets can be recognized since they will remain relatively fixed in amplitude while the sea spikes come and go. |
Isolation can also be increased by transmitting on an orthogonal polarization to that received. Providing they are operating with linear gain, there are no adverse effects from radar sidelobe interrogation. However, at close ranges, the signal from the main beam of the radar may saturate within the RTE, effectively enhancing the levels of the RTE received signal through the radar sidelobes. |
For a finite array the properties vary with location of the element within the array. In some arrays, dummy elements are placed on the periphery so as to provide the elements near the edge with an environment more like those located in the interior. Although there have been many di!Terent kinds of radiators used in phased arrays, the dipole. |
PRODUCTS ARE GENERATED WHICH REDUCE THE ECHOS MATCHED |
Houze, Jr., and J. D. Locatelli: Real-Time Wind Measurement in Extratropical Cyclones by Means of Doppler Radar, /. |
and T. F. Bush: Corn Growth as Monitored by Rada1. |
2!$!2 $)')4!, 3)'.!, 02/#%33).' Óx°ÓÇ #OMPARED TO &)2 FILTERS ))2 FILTERS OFFER SEVERAL ADVANTAGES )N GENERAL THEY REQUIRE LESS PROCESSING AND MEMORY TO IMPLEMENT SIMILAR FUNCTIONS )T IS ALSO EASIER TO IMPLE |
When tile wind is blowing toward the radar tlie dpproacliing-wavc spectral line IS the larger of the two. When the wind is blowing away from the radar, the receding-wave spectral line is the larger When the wind IS blowing perpendicular to the direction of the radar beam, the two spectral lines are equal. Thus the relative magnitude of the two major components of the doppler spectrum can provide a measure of the direction of the wind. |
● The combiner should have RF isolation among ports, such that failed modules do not affect the load impedances or combining efficiency for the remaining functioning modules. ● The combiner should provide a controlled RF impedance to the amplifier modules, such that the amplifier characteristics are not degraded. ● The dissipated power capability of the power combiner terminations should be suf - ficient to accommodate any combination of power amplifier failures. |
BASED MEASUREMENTS 4HUS BEING ABLE TO MEASURE STRONG PRECIPITATION ECHOES AT SHORT RANGE AND ALSO WEAK PRECIPITATION ECHOES AT LONG RANGE REQUIRES RADAR RECEIVERS HAVING A TOTAL DYNAMIC RANGE OF n D" WHEREAS MEASURING WEAK ECHOES IN THE PRESENCE OF STRONG GROUND CLUTTER REQUIRES AS LARGE AN INSTANTA |
The calibrations shown in Figure 16.12 are incomplete without knowing the antenna patterns and absolute gains. Since accurate gain measurements are difficult, absolute calibrations may be made by comparing received signals (with proper rela - tive calibration) from the target being measured and from a standard target . Standard targets may be metal spheres, Luneburg-lens reflectors, metal plates, corner reflectors, or active radar calibrators (ARCs—actually repeaters).84,85 Of the passive calibrators, the Luneburg-lens reflector is best because it has a large cross section for its volume and has a very wide pattern so that alignment is not critical. |
MAP |
COST 643 SYSTEMS STILL COMMONLY USE SUBSYSTEMS INTENDED FOR SHIPBORNE USE GIVING GOOD COST SAVINGS COMPARED TO CUSTOM |
vi. Adjust the orientation of the PPI so that the upward direction on the tube face is the heading of the aircraft. This is effected by setting the track line onthe Perspex screen to zero, setting the switch on the heading control unit to manual, and turning the setting knob until the course marker lies under the track line. |
9.26. Examples ofRadomes.—Types ofradomes vary greatly insize, shape, and method ofconstruction. Attention iscalled toafew repre- sentative radomes. |
Patent No. 3,797,017, Mar. 12, 1974. |
Atthesametime,moisture isaddedfromthesea toproduce amoisture gradient. Thisformofanomalous propagation overtheseatendstobe moreprominent ontheleeward sideoflandmasses.Ducting occursduringeitherthedayor nightandcanlastforlongperiodsoftime.Itismostlikelytooccur,however, inthelate afternoon andevening whenthewarmafternoon airdriftsoutoverthesea..B Thusthecharacter ofducting' islikelytodifferoverlandandsea.Landmasseschange temperature muchmorequickly than'does thesea.Asaresult,thereismuchmoreofadiurnal variation ofducting overlandthanoversea,whereitislikelytobemorecontinuous and widespread.32 .Superrefracting groundductsmayalsobeproduced bythediverging downdraft undera thunderstorm.3!Therelatively coolairwhichspreadsoutfromthebaseofathunderstorm resultsinatemperature inversion inthelowestfewthousand feet.Themoisture gradient is alsoappropriate fortheformation ofaduct.Ductformation bythunderstorms maynotbeas frequent asotherducting mechanisms, butitisofimportance sinceitmaybeusedasameans ofdetecting thepresence ofastorm.Anoperator carefully watching aradardisplaycanddcct thepresence ofastormbythesuddeninc'rease inthenumberandrangeofgroundtargets.The conditions appropriate tothe'formation Iofathunderstorm ductareshort-lived andhavea timeduration oftheorderof'perhaps 30minto1h. Withtheexception ofthunderstorms, ducting isessentially afine-weather phenomenon. |
Thesumsignalhashigher sidelobes because theseparation between thephasecentersoftheseparate antennas islarge.(Thesehighsidelobes aretheresultof gratinglohes.similartothoseproduced inphasedarrays.)Theproblem ofhighsidelobes can hereduced byoverlapping theantenna apertures. Withreflector antennas, thisresultsinaloss ofanglesensitivity andantenna gain. 5.5TARGET-REFLECTION CHARACTERISTICS ANDANGULAR ACCURACyJo.41.Q5 Theangular accuracy oftracking radarwillbeinfluenced bysuchfactorsasthemechanical properties oftheradarantenna andpedestal, themethodbywhichtheangular position ofthe antenna ismeasured, thequalityofthes~osysteQ'l,thestability oftheelectronic circuits, the noiselevelofthereceiver, theantenna beamwidth, atmospheric fluctuations, andthereflection characteristics ofthetarget.Thesefactorscandegrade thetracking accuracy bycausingthe antenna beamtofluctuate inarandom manner aboutthetruetargetpath.Thesenoiselike fluctuations aresometimes calledtracking noise,orjitter. |
This delay is quantized by a range gate pull off (RGPO) device. A range gate stealer system linearly delays the quantized signal in order to generate a constant range-rate false target. The joint effect of phase and delay quantization in DRFM can be analyzed as reported in Greco, Gini, and Farina.26 Other artifacts in the deception signals can be introduced by imperfections in the down-up conversion and demodulation/modulation of the signal performed in the DRFM device. |
This is known as target classification. The time delay between the transmission of the radar signal and the receipt of an echo is a measure of the distance, or range, to the target. The range measurement is usually the most significant a radar makes. |
Any use is subject to the Terms of Use as given at the website. Synthetic Aperture Radar. 17 .36 RADAR HANDBOOK 6x9 Handbook / Radar Handbook / Skolnik / 148547-3 / Chapter 17 34. R. |
1, pp. 272-293, 1958. 42. |
Improved Delay Line Technique Study, RADC Tech. Rept. RADC-TR-65-45, May 1965. |
N.: Use of Bistatic Radar Techniques to Improve Resolution in the Ver- tical Plane, IEE Electron. Lett., vol. 4, pp. |
The nature of the circuit may also demand that the lagging edge be vertical, to produce an imstantaneous cut-off. Such a wave-form is produced in the transmitter modulator, the pulse of energy is broadcast, and a signal received by the radar receiver. Now there is one impor- tant difference between a radar and a broadcast radio receiver. |
into the holes of the hole-and-slot resonators to change the inductance of the resonant circuit. A tuner that consists of a series of rods inserted into each cavity resonator so as to alter the inductance is called a crown-of-thorns tuner, or a sprocket t1111cr. The amount of mechanical motion of the tuning element need not be large (perhaps a fraction of an inch at L band) to tune the frequency over a 5 to 10 percent frequency range. |
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