MotRadar System Principles
Transcript of MotRadar System Principles
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By: Motuma Muktar
Radar System Principles
andApplications
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Outline
Definition Historical Background
Radar Basics Radar Equation
Doppler Effect
Polarization Limiting Factors
Radar Sets and Devices
Components of Radar System
Advantages Applications
Summary
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Definition
Radar: acronym for Radio Detection and Ranging.
an electronic and electromagnetic system that uses radio waves to detect
and locate objects.
It operates by transmitting a particular kind of radio
frequency waveform and detecting the nature of the reflected
echo.
When radio waves strike an object, some portion is reflected,
and some of this reflected energy is returned to the radar
set, where it is detected.
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Historical Background
In 1886, Heinrich Hertz showed that radio waves could bereflected from solid objects.
The German Christian Huelsmeyer was the first to use
radio waves to detect "the presence of distant metallic
objects". In 1904 he demonstrated the feasibility ofdetecting a ship in dense fog, but not its distance.
After passing through many stages, full radar evolved as a
pulsed system, and the first such elementary apparatus was
demonstrated in December 1934 by the American RobertM. Page, working at the Naval Research Laboratory.
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Radar Basics
A radar system has a transmitter that emits radio wavescalled radar signals in predetermined directions.
When these come into contact with an object they are
usually reflected and/or scattered in many directions.
Radar signals are reflected especially well by materials ofconsiderable electrical conductivity.
If the object is moving either closer or farther away, there is
a slight change in the frequency of the radio waves, due to
the Doppler Effect.
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Cont
Radar receivers are usually, but not always, in the samelocation as the transmitter.
Although the reflected radar signals captured by the
receiving antenna are usually very weak, these signals can
be strengthened by the electronic amplifiers. The weak absorption of radio waves by the medium
through which it passes is what enables radar sets to detect
objects at relatively-long range.
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Cont
Radar waves scatter in a variety of ways depending on thesize (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 is reflected by amirror.
If the wavelength is much longer than the size of the target, the
target may not be visible due to poor reflection.
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Radar Equation
The power Prreturning to the receiving antenna is given by
Pt = transmitter power
Gt = gain of the transmitting antenna
Ar= effective aperture (area) of thereceiving antenna
= radar cross section, or scattering
coefficient, of the target
F = pattern propagation factor
Rt = distance from the transmitter to the
targetRr= distance from the target to the receiver.
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Doppler Effect The apparent frequency (f) of the wave changes with the relative
position of the target. Doppler equation is stated as:
The change in phase of the return signal is often used instead of thechange in frequency.
Only the radial component of the speed is available. when a target is moving at right angle to the radar beam, it has no velocity
one parallel to it has maximum recorded speed
vobs= the radial speed of
the observer
vs= the radial speed ofthe targetf0 =frequency of wave :
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Polarization
In the transmitted radar signal, the electric field isperpendicular to the direction of propagation. This direction
of the electric field is the polarization of the wave.
Radars use horizontal, vertical, linear and circular
polarization to detect different types of reflections. E.g. Circular polarization is used to minimize the interference caused by
rain.
Linear polarization returns usually indicate metal surfaces.
Random polarization returns usually indicate a fractal surface, such
as rocks or soil, and are used by navigation radars.
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Limiting Factors
Beam path and range
Noise
Interference
Clutter
Jamming
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Limiting Factors
Beam path and range
Noise
Interference
Clutter
Jamming
The radar beam would follow
linear path in vacuum
curved path in the
atmosphereMaximum range limiting factors
LOS
The maximum non-
ambiguous range
Radar sensitivity and
power of the returned signal
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Limiting Factors
Beam path and range
Noise
Interference
Clutter
JammingNoise is generated by:
Electronic components
natural thermal radiation
of the background scene
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Limiting Factors
Beam path and range
Noise
Interference
Clutter
Jamming
The ability of the radar system to
overcome these unwantedsignals defines its signal-to-noise
ratio (SNR).
A higher system's SNR is
required .
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Limiting Factors
Beam path and range
Noise
Interference
Clutter
Jamming
Includes ground returns, sea
returns, weather, buildings, birds
and insects.
It depends on the function of the
radar.
Types of Clutter:
Surface clutter
Volume clutter
Point clutter
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Limiting Factors
Beam path and range
Noise
Interference
Clutter
Jamming
It refers to radio frequency signals
originating from sources outside the
radar, transmitting in the radar's
frequency
mask targets of interest.
It is problematic to radar because the jamming signal only
needs to travel one-way
the radar echoes travel two-
ways
Therefore radar signal is
significantly reduced in powerby the time they return to the
radar receiver
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Radar Sets and Devices
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Classification of Radar System Based on Technology
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Cont
Based on the Designed use
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Radar Signal Processor
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Components of Radar System
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Advantage of Radar
It provides superior penetration capability through any type ofweather condition
It can be used in the day or night time.
It uses electromagnetic wave that does not require a medium
like Sonar (that uses water) so can be used in space and air. Radar can be long range and the wave propagate at the speed of
light rather than sound (like with sonar).
It is less susceptible to weather conditions compared with
Lasers.
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Applications
Military purposes: to locate air, ground and sea targets.
Aviation : to warn from obstacles in or approaching their
path and give accurate altitude readings.
Marine radars are used to measure the bearing and distance
of ships to prevent collision with other ships
Meteorologists use radar to monitor precipitation
Geologists use specialized ground-penetrating radars to
map the composition of the Earth's crust.
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Summary
The transmission and reception of radio waves is thefundamental operation of radar waves.
Many properties and phenomena of radio waves are crucial
to the operation of the radar system.
The Earths atmosphere plays a central role in radaroperation, as it is the medium of propagation for the radio
waveforms.
The Doppler Effect also plays a vital role in practical radar
systems. Radar has numerous applications including air traffic
control, meteorology, and military applications.
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References
Wikipedia http://en.wikipedia.org/wiki/Radar
http://www.radartutorial.eu/
Michael O. Kolawole,Radar System, Peak Detection and Tracking,
1st Edition, 2003
Lav Varshney, Technical Report,Radar System Components and
System Design, November 22, 2002
Reintjes, J. Francis and Godfrey T. Coate, Principles of Radar. New
York: McGraw-Hill, 1952.
Skolnik, Merrill I.,Introduction to Radar Systems. New York:
McGraw-Hill, 1980. Thomas, Daniel, Signal Processing. Radar 101 Lecture Series.
Syracuse Research Corporation, Syracuse. 31 Oct. 2001.
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Thank You