This document provides an overview of radar technology. It discusses key radar concepts like reflection, polarization, distance and speed measurement, positioning, and the radar equation. It also describes different radar frequency bands and specific radar systems like AESA, Doppler weather radar, cloud radar, NEXRAD, passive radar, pulse-Doppler radar, and synthetic aperture radar. Radar uses radio waves to detect and locate objects at a distance by transmitting pulses and analyzing the echo signal.

1. RADAR COMMUNICATION
ABSTRACT
This long range radar antenna (approximately 40m (130ft) in
diameter) rotates on a track to observe activities near the horizon.
RADAR is an acronym for Radio Detection And Ranging or
Radio Angle Detection And Ranging. It is a system used to
detect, range (determine the distance of), and map objects such as
aircraft and rain. Strong radio waves are transmitted, and a receiver
listens for any echoes. By analysing the reflected signal, the reflector
can be located, and sometimes identified. Although the amount of
signal returned is tiny, radio signals can easily be detected and
amplified.
Radar radio waves can be easily generated at any desired strength, detected at even tiny
powers, and then amplified many times. Thus radar is suited to detecting objects at very

2. large ranges where other reflections, like sound or visible light, would be too weak to
detect.
INTRODUCTION
In 1887, the German physicist Heinrich Hertz began experimenting with radio
waves in his laboratory. He found that radio waves could be transmitted through different
types of materials, and were reflected by others. The existence of electromagnetic waves
was predicted earlier by James Clerk Maxwell, but it was Hertz who first succeeded in
generating and detecting radio waves experimentally.
The scientists named CHRISTIAN HUELSMEYER , NIKOLA TESLA,
A.H.TAYLOR , L.C.YOUNG and ROBERT WATSON – WATT researched
and developed the fundamentals of RADAR technology in 1900’s.
PRINCIPLES
Reflection

3. Description
Electromagnetic waves reflect (scatter) from any large change
in the dielectric or diamagnetic constants. This means that a
solid object in air or vacuum, or other significant change in
atomic density between object and what's surrounding it, will
usually scatter radar (radio) waves. This is particularly true of
electrically conductive materials such as metal and carbon
fiber, making radar particularly well suited to the detection of
aircraft and ships. Radar absorbing material, containing
resistive and sometimes magnetic substances, is used on
military vehicles to reduce radar reflection. This is the radio
equivalent of painting something a dark color.
Radar waves scatter in a variety of ways depending on the size (wavelength) of the radio
wave and the shape of the target. If the wavelength is much shorter than the target's size,
the wave will bounce off in a way similar to the way light bounces from a mirror. If the
wavelength is much longer than the size of the target, the target is polarized, like a dipole
antenna. This is described by Rayleigh Scattering (like the blue sky). When the two
length scales are comparable, there may be resonances. Early radars used very long
wavelengths that were larger than the targets and received a vague signal, whereas some
modern systems use shorter wavelengths (a few centimeters or shorter) that can image
objects as small as a loaf of bread or smaller.
Radio waves always reflect from curves and corners, in a way similar to glint from a
rounded piece of glass. The most reflective targets for short wavelengths have 90° angles
between the reflective surfaces. A surface consisting of three flat surfaces meeting at a
single corner, like the corner on a block, will always reflect directly back at the source.
These so-called corner cubes are commonly used as radar reflectors to make otherwise
difficult-to-detect objects easier to detect, and are often found on boats in order to
improve their detection in a rescue situation and reduce collisions. For generally the same
reasons objects attempting to avoid detection will angle their surfaces in a way to
eliminate inside corners and avoid surfaces and edges perpendicular to likely detection

4. directions, which leads to "odd" looking stealth aircraft. These precautions do not
completely eliminate reflection because of diffraction, especially at longer wavelengths.
Electromagnetic waves do not travel well underwater; thus for underwater applications,
sonar, based on sound waves, has to be used instead of radar.
Polarization
Polarization is the direction that the wave vibrates. Radars use horizontal, vertical, and
circular polarization to detect different types of reflections. For example, circular
polarization is used to minimize the interference caused by rain. Linear polarization
returns usually indicate metal surfaces, and help a search radar ignore rain. Random
polarization returns usually indicate a fractal surface like rock or dirt, and are used by
navigational radars.
Brightness can indicate reflectivity as in this 1960 weather
radar image. The radar's frequency, polarization, and
receiver determine what it can observe.
Distance measurement
Transit time
The easiest way to measure the range of an object is to broadcast a short pulse of radio
signal, and then time how long it takes for the reflection to return. The distance is one-
half the product of round trip time (because the signal has to travel to the target and then
back to the receiver) and the speed of the signal. Where c is the speed of
light in a vacuum, and τ is the round trip time. For RADAR the speed of signal is the
speed of light, making the round trip times very short for terrestrial ranging. For this

5. reason accurate distance measurement was difficult until the introduction of high
performance electronics, with older systems being accurate to perhaps a few percent.
The receiver cannot detect the return while the signal is being sent out – there is no way
to tell if the signal it hears is the original or the return. This means that a radar has a
distinct minimum range, which is the length of the pulse divided by the speed of light,
divided by two. In order to detect closer targets you have to use a shorter pulse length.
A similar effect imposes a specific maximum range as well. If the return from the target
comes in when the next pulse is being sent out, once again the receiver cannot tell the
difference. In order to maximize range, one wants to use longer times between pulses, the
inter-pulse time.
Frequency modulation
Another form of distance measuring radar is based on frequency modulation. Frequency
comparison between two signals is considerably more accurate, even with older
electronics, than timing the signal. By changing the frequency of the returned signal and
comparing that with the original, the difference can be easily measured.
This technique can be used in radar systems, and is often found in aircraft radar
altimeters. In these systems a "carrier" radar signal is frequency modulated in a
predictable way, typically varying up and down with a sine wave or sawtooth pattern at
audio frequencies. The signal is then sent out from one antenna and received on another,
typically located on the bottom of the aircraft, and the signal can be continuously
compared.
Since the signal frequency is changing, by the time the signal returns to the aircraft the
broadcast has shifted to some other frequency. The amount of that shift is greater over
longer times, so greater frequency differences mean a longer distance, the exact amount
being the "ramp speed" selected by the electronics. The amount of shift is therefore
directly related to the distance travelled, and can be displayed on an instrument. This
signal processing is similar to that used in speed detecting doppler radar. See the article
on continuous wave radar for more information.

6. Speed measurement
Speed is the change in distance to an object with respect to time. Thus the existing system
for measuring distance, combined with a little memory to see where the target last was, is
enough to measure speed. At one time the memory consisted of a user making grease-
pencil marks on the radar screen, and then calculating the speed using a slide rule.
However there is another effect that can be used to make much more accurate speed
measurements, and do so almost instantly (no memory required), known as the Doppler
effect. Practically every modern radar uses this principle in the pulse-doppler radar
system. It is also possible to make a radar without any pulsing, known as a continuous-
wave radar (CW radar), by sending out a very pure signal of a known frequency. Return
signals from targets are shifted away from this base frequency via the Doppler effect
enabling the calculation of the speed of the object relative to the radar.
POSITION MEASUREMENT
Radio signals broadcast from a single antenna will spread out in all directions, and
likewise a single antenna will receive signals equally from all directions. This leaves the
radar with the problem of deciding where the target object is located.
Early systems
Early systems tended to use omni-directional broadcast antennas, with directional
receiver antennas which were pointed in various directions. For instance the first
system to be deployed, Chain Home, used two straight antennas at right angles for
reception, each on a different display.
One serious limitation with this type of solution is that the broadcast is sent out in all
directions, so the amount of energy in the direction being examined is subject to the
inverse-square law. To get a reasonable amount of power on the "target", the broadcast
should also be steered. More modern systems used a steerable parabolic "dish" to create a
tight broadcast beam, typically using the same dish as the receiver. Such systems often
combined two radar frequencies in the same antenna in order to allow automatic steering,
or radar lock.

7. Not all radar antennas must rotate to scan the sky.
RADAR EQUATION
The amount of power Pr returning to the receiving antenna is given by the radar equation:
Where
Pt = transmitter power,
Gt = gain of transmitting antenna,
Ar = effective aperture (area) of receiving antenna,
σ = Radar Cross Section, or scattering coefficient of target,
Rt = distance from transmitter to target,
Rr = distance from target to receiver.
In the common case where the transmitter and receiver are at the same location, Rt = Rr
and the term Rt² Rr² can be replaced by R4, where R is the range. This yields:
This shows that the received power declines as the fourth power of the range, which
means that the reflected power from distant targets is very, very small.
Other mathematical developments in radar signal processing include time-frequency
analysis (Weyl Heisenberg or wavelet), as well as the chirplet transform which makes use
of the fact that radar returns from moving targets typically "chirp" (change their
frequency as a function of time, as does the sound of a bird or bat).

8. FREQUENCY BANDS
The traditional band names originated as code-names during World War II and are still in
military and aviation use throughout the world in the 21st century. They have been
adopted in the United States by the IEEE, and internationally by the ITU. Most countries
have additional regulations to control which parts of each band are available for civilian
or military use.
Other users of the radio spectrum, such as the broadcasting and electronic
countermeasures (ECM) industries, have replaced the traditional military designations
with their own systems.
Radar Frequency Bands
Band Frequency Wavelength
Notes
Name Range Range
HF 3-30 MHz 10-100 m coastal radar systems;'high frequency'
'P' for 'previous', applied retrospectively to early radar
P < 300 MHz 1 m+
systems
VHF 50330MHz 0.9-6 m very long range,groundpenetrating;'veryhighfrequency'
300-1000 Very long range (e.g. ballistic early warning), ground
UHF 0.3-1 m
MHz penetrating; 'ultra high frequency'
long range air traffic control and surveillance; 'L' for
L 1-2 GHz 15-30 cm
'long'
terminal air traffic control, long range weather, marine
S 2-4 GHz 7.5-15 cm
radar; 'S' for 'short'
a compromise (hence 'C') between X and S bands;
C 4-8 GHz 3.75-7.5 cm
weather
X 8-12 GHz 2.5-3.75 cm missile guidance, marine radar, weather; in the USA the
narrow range 10.525GHz ±25MHz is used for airport

9. radar.
high-resolution mapping, satellite altimetry; frequency
Ku 12-18 GHz 1.67-2.5 cm
just under K band (hence 'u')
Mapping, short range, airport surveillance; frequency
just above K band (hence 'a') Photo radar, used to
Ka 27-40 GHz 0.75-1.11 cm
trigger cameras which take pictures of license plates of
cars running red lights, operates at 34.300 ± 0.100 GHz.
mm 40-300 GHz 1 - 7.5mm 'millimetre' band, subdivided as below
V 40-75 GHz 4.0 - 7.5 mm
used as a visual sensor for experimental autonomous
W 75-110 GHz 2.7 - 4.0 mm
vehicles, high-resolution meterological observation
SPECIFIC RADAR SYSTEMS
Active Electronically Scanned Array (AESA)
An Active Electronically Scanned Array (AESA) is a revolutionary type of radar
whose transmitter and receiver functions are composed of numerous small
transmit/receive (T/R) modules that each scan a small fixed area, negating the need for a
moving antenna. AESA radars feature short to instantaneous (millisecond) scanning rates
and have desirable low-probability of intercept characteristics
Continuous-wave radar
Continuous-wave radar system is a radar system where a continuous wave is transmitted
by one antenna and a second receives the radio energy reflected from an object.
Doppler radar as weather radar
Doppler radar uses the Doppler Effect to return additional information from a radar
system. The Doppler Effect shifts the frequency of the radar beam due to movement of
the "target", allowing for the direct and highly accurate measurement of speeds. Doppler

10. radars were originally developed for military radar systems, but have since become a part
of almost all radar systems, including weather radar and radar guns for traffic police and
sports
Millimeter cloud radar
The millimeter wave cloud radar (MMCR) is a remote sensing instrument that transmits a
radar pulse directly overhead to determine the tops and bottoms of clouds. It can also
serve as a type of Doppler radar in measuring up and down particle movements within a
cloud. Values that the radar measures are Doppler velocity, radar reflectivity, and spectral
width.
NEXRAD
NEXRAD Radar at NSSL
NEXRAD or Nexrad (the next-generation radar) is a network of Doppler radars
operated by the National Weather Service, an agency of NOAA, the National Oceanic
and Atmospheric Administration, in the United States. NEXRAD detects precipitation
and atmospheric movement or wind. It returns data which when processed can be
displayed in a mosaic map which shows patterns of precipitation and its movement. The
radar system operates in two basic modes, selectable by the operator: a slow-scanning

11. "clear-air mode" for analyzing air movements when there is little or no activity in the
area, and a "precipitation mode" with a faster scan time to do traditional storm tracking.
Passive radar
Passive Radar is type of radar system which uses one or more receivers, but lacks an
active transmitter. The system detects ambient radio signals emanating from nearby radio
transmitters. The receiver is either bistatic or multistatic, since it is positioned elsewhere.
The system is not restricted to one receiver—several receiver systems may be operated in
conjunction with one or many transmitters.
Pulse-Doppler radar
Radar gun traffic and sports radars
U.S. Army soldier uses a radar gun to catch speeding
violators at Tallil Air Base, Iraq.
A radar gun is a small Doppler radar used to detect the
speed of objects. A radar gun does not return position or
power information. It relies on the Doppler Effect applied to
a radar beam to measure the speed of objects it is pointed at.
Radar guns may be hand-held or vehicle-mounted. Common uses include traffic speed
law enforcement, and measuring the speed of balls in sports.
Secondary surveillance radar (SSR).

12. Synthetic aperture radar
The surface of Venus, as imaged by the Magellan probe using SAR,
Synthetic aperture radar (SAR) is a form of radar in which sophisticated post-
processing of radar data is used to produce a very narrow effective beam. It can only be
used by moving instruments over relatively immobile targets, but it has seen wide
applications in remote sensing and mapping.
X-band radar