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Antenna Measurements: Dihedrals, ground targets and antenna beam patterns AMS Radar Calibration Workshop Albuquerque, New Mexico 13-14 January 2001 Ronald E. Rinehart University of North Dakota Grand Forks, ND 58202-9006 Voice: 701-777-2183; fax: 701-777-5032 email: rinehart@aero.und.edu or radarwx@aol.com 1/19/1 1
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Other speakers in this session: Ken Tapping John Lutz Dave Brunkow & John Hubbe Dick Doviak 1/19/1 2
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Speakers in this session: 1/19/1 3
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Beware of the hazard associated with this talk: 1/19/1 4
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Growing a crop of antennas at EEC, Enterprise, AL 1/19/1 5
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More antennas growing in New Mexico 1/19/1 6
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Why we need to know antenna parameters: Point target radar equation: Meteorological target radar equation: 1/19/1 7
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receiver transmitter modulator master clock display signal processor/ computer r 1/19/1 8
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receiver transmitter modulator master clock display signal processor/ computer r 1/19/1 9
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Here’s what we think happens: Here’s what actually happens: And it gets even worse! A radar’s view of a storm: 1/19/1 10
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Antenna characteristics than need to be measured: gain mainlobe sidelobes complete pattern beamwidth 1/19/1 11
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How can we measure beamwidth, gain and antenna beam pattern? Antenna range Signal generator/horn Standard target Secondary-standard target Sun 1/19/1 12
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Use of antenna range: Requires moving the antenna to the antenna range. Expensive Time-consuming Excellent results 1/19/1 13
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Signal Generator & Horn Aim antenna at S/G and horn Scan antenna in azimuth & elevation S/G needs to be in far field (?): Far field distance = 2D 2 / D = antenna diameter, = wavelength Examples of two antennas: C-band, 3.66 m (12 ft) --> 495 m ~0.5 km S-band, 8.53 m (28 ft) --> 1360 m ~1.5 km Excellent results 1/19/1 14
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Standard Targets Sphere Tethered Lots of work, good results Dihedral Surveyed position Gives gain, azimuth & range Can also give beam pattern Quite convenient; good results 1/19/1 15
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Gain using standard target - sphere Use sphere on tethered balloon at some location 3- 15 km from radar. Location must be free of ground clutter. Scan target in range and azimuth and use peak value recorded. Use point radar equation to calculate gain. Backscattering cross-sectional area of sphere is either geometric or resonant region. if resonant, use Fig. 4.2, pg. 72, Radar for Meteorologists, Fig 4.2, pg. 37, Battan, 1973: Radar Observation of the Atmosphere; 1/19/1 16
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…a pet peeve: 1/19/1 17
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Antenna gain using dihedral target Mount dihedral target 5-15 km from radar Avoid nearby ground clutter. Using motorized nodding mechanism, allow dihedral to nod up and down through a position normal to beam. Aim antenna in azimuth and elevation for peak signal. Record signal amplitude and use strongest found. Calculate gain using radar equation for point targets. 1/19/1 19
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Nodding Dihedral Top view Side view Perspective view Nodding action 1/19/1 20
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Side view of dihedral target Pivot point Eccentric cam Motor 1/19/1 21
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Working on the dihedral Bill Bradley (on pole) Greg Muir observing. Looking west; radar located NW 1/19/1 23
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Signal from dihedral while nodding (+ calibration signal) 1/19/1 24
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Advantages of dihedral Excellent way to get antenna gain Good check on range and azimuth of radar Inexpensive to operate (once installed) Not labor intensive Quick: can get G within 10 min or so Can use it without nodding once set then it’s even faster 1/19/1 25
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Secondary Standard Targets Strong, isolated radio towers, water towers, or buildings Beware of changes Useful for quickly monitoring overall system “health” Check of receiver, transmitter, azimuth and range 1/19/1 1
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Sun Useful for measuring antenna gain Too weak to get a full beam pattern Also, not quite a point target, so more difficult to use. http://134.153.112.105/t-se-anim.gif 1/19/1 2
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Antenna the transducer that converts the electrical signal into an electromagnetic signal the interface between the hardware and the medium carrying the EM signal consists of actual antenna and a reflector 1/19/1 3
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Reflector parabolic in cross-section focus reflector 1/19/1 4
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Reflector rays from focus are reflected parallel into space 1/19/1 5
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Reflector rays from space are reflected back to the focal point 1/19/1 6
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Antenna Actual antenna is either a horn or a dipole: half-wavelength dipole antenna sub-reflector Feed horn 1/19/1 7
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Feedhorn Need to connect feedhorn to the rest of the system somehow. 1/19/1 8
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Alternate arrangements Off-set Parabolic 1/19/1 9
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Feedhorn and waveguide; tabs for supports 1/19/1 10
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NCAR CP-2 dual- polarization antenna 1/19/1 12
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Dual- polarization feedhorn and antenna ( CSU- CHILL) http://radarmet.atmos. colostate.edu/CHILL/Pix.html 1/19/1 13
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Dual-polarization feed on EEC radar 1/19/1 14
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Reflector cross-section (viewed from front or back) Circular “orange peel” vertical (height-finding) horizontal (azimuth finding) 1/19/1 15
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Reflector Directs signal into space, i.e., focuses it in the desired direction Generally parabolic in shape Larger antennas give smaller beamwidths (for the same wavelength signal) Higher frequencies require smaller antennas for the same beamwidth aircraft usually use X or C band ground-based radars usually use S or C band 1/19/1 16
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Isotropic antenna An isotropic antenna radiates equally in all directions Examples: the sun and other stars a candle (except downward) fireworks or explosions Real antennas are never truly isotropic 1/19/1 17
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The advantage of using a reflector Reflectors focus energy into a particular direction. Reflectors make the energy at some point stronger than it would have been otherwise. Reflectors allow us to determine direction to a target. 1/19/1 18
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Intensity at target without reflector 1/19/1 19
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Intensity at target with reflector Reflector 1/19/1 20
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Antenna gain The gain of antenna is the ratio of the power at a point when an antenna is used to that from an isotropic antenna at the same point. 1/19/1 21
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Gain of real antennas isotropic1.0 simple dipole1.5 small circular parabolic4000 UND (12-ft diameter, C-band)23700 WSR-88D (28-ft dia., S-band)31600 1/19/1 22
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Logarithmic units Because some parameters vary over several orders of magnitude, it is sometimes convenient to convert to a logarithmic scale: logarithmic power ratio [dB] = 10log 10 (p 1 /p 2 ) where the logarithmic units are decibels. 1/19/1 23
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Logarithmic gain where p 1 is the (linear) power with the antenna, p 2 is the (linear) power of an isotropic antenna, g is the linear gain (unitless number) and G is the logarithmic gain of the antenna measured in decibels. p 1 and p 2 need to be measured or converted to the same units; milliwatts are frequently used. 1/19/1 24
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Gain of real antennas (logarithmically) isotropic 0 dB simple dipole1.8 dB small circular parabolic 36 dB UND 12 ft antenna43.75 dB WSR-88D 28-ft antenna45 dB 1/19/1 25
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Antenna beamwidth The angular width of an antenna pattern The angular width where the power density is 1/2 that on the axis of the beam. half-power point or 3-dB point 1/19/1 1
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Antenna beamwidth Antenna beam axis Double the angle to get the half-power point antenna beamwidth. Measure power on beam axis Measure angle from axis to half-power point (at the same range). 1/19/1 2
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Gain vs. Beamwidth Gain and beamwidth are related by equation (Battan, 1973): where g is the linear gain of the antenna, k 2 depends upon the shape of the antenna. k 2 = 1 for circular reflectors. and are the horizontal and vertical beamwidths, respectively. Beamwidths must be measured in radians. 1/19/1 3
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Antenna sidelobes There are no perfect antennas! All antennas have antenna patterns which include main lobe side lobes back lobes 1/19/1 4
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Top-hat beam pattern Simplest assumption - no power at all until in the beam pattern, then uniform power. Power Relative angle 1/19/1 5
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Top-hat pattern (in polar coordinates) Antenna beam axis 1/19/1 6
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Gaussian beam pattern Relative angle Power 1/19/1 7
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Gaussian beam pattern (in polar coordinates) Antenna beam axis 1/19/1 8
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Simple sidelobes - CPS-9 0 1 2 3 4 5 Relative angle (deg) Relative gain (dB) 0 -10 -20 -30 -40 1/19/1 9
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CPS-9 Gain in Polar Coordinates 1/19/1 10
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Examples of real antennas NCAR CP-2 S- and X-band dual- wavelength radar Lincoln Lab FL2 S-band radar UND C-band radar 1/19/1 11
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Notice (20 years too late?) Slight (~0.3°) offset in S- and X- band mainlobe pointing directions! Different sidelobes Different mainlobe widths 1/19/1 13
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Using ground targets to measure beam patterns Pick strong target fairly close by. If needed, use very strong target for sidelobes and somewhat weaker target for mainlobe If target saturates receiver, top of mainlobe will be lost. If target is too weak, sidelobes are lost. Scan with resolution about a third to fifth of the beamwidth in azimuth & elevation. 1/19/1 18
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UND radar beam pattern Used 2000-ft radio tower located 67 km toward SSW. Scanned with 0.2° average interval in azimuth and 0.2° elevation steps Note: beamwidth is 0.97° 1/19/1 19
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UND radar beam pattern Adjusted raw azimuths to the nearest 0.2° Found CW vs. CCW azimuth offset Adjusted one of these to agree with the other. Kept CW data the same, adjusted CCW 0.2° CCW to reduce offset to zero). It would be better to use calculated azimuth to target as standard. Get from GPS positions. 1/19/1 20
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Procedure for getting pattern Scan target & record data Edit data to common angles & remove spurious targets Smooth data, Correct for hysteresis Plot pattern 1/19/1 21
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Conclusions: Knowledge of antenna characteristics will make you a better meteorologist (and better person). Adopt a pet target or two and use them occasionally to check on the health of your system Be aware that what you see on a radar is biased by the antenna beam pattern. 1/19/1 25
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References added after RADCAL Workshop: Rinehart, R. E., P. J. Eccles, 1976: Use of a nodding dihedral target for antenna gain measurements. 17 th Conf. on Radar Meteorology, Seattle, WA, pp 66-71. Rinehart, R. E., and Charles L. Frush, 1983: Comparison of antenna beam patterns obtained from near-field test measurements and ground target scans. 21 st Radar Meteorology Conf., Edmonton, Canada, pp 291- 295. Rinehart, R. E., and John D. Tuttle, 1981: A technique for determining antenna beam patterns using a ground target. 20 th Conf. on Radar Meteorology. Boston, MA, pp 672-675. 1/19/1 26
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