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Atmospheric RADARSignal Processing
E X T E R N A L G U I D E :
DR. T.V.C. SA RMA,
( S C I E N T I S T / E N G I N E E R - S G )
NATIONAL ATMOSPHERICRESEARCH LABORATORY,
DEPARTMENT OF SPACE
INTERNAL GUIDE :
M R . R A L P H T H A N G A R A J ,
V E L L O R E I N S T I T U T E O FT E C H N O L O G Y,
S E N S E D E PA RT M E N T
( A S S O C I AT E P R O F E S S O R )
PRE
B. L
1 M
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Outline
IntroductionMST radar
Research proposal
Literature survey
ontinuous !ave radar and pulse radar Ran"e
Ran"e resolution#ulse co$pression % Types
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Introduction RADAR% Radio Detection and Ran"in"Radars "enerally operated at &re'uency a(out ))*M+, %-.G+,
/+0 1 -*M % -**M+,
U+0 1 -**M % -G+,
S+0 1 -G % -*G+, T!o types o& radar syste$s
23 ontinuous 4ave Radar
)3 #ulse radar
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MST Radar
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Research Proposal The aim is transmitted wave is back scattered by radio refractive
index irregularities due clear air turbulence(CAT) towards the radarand it is received by the same antenna in the case of Monostaticsystem by using duplexer
The received echo is processed through superhetrodyne receiverfollowed by quadrature detection with !"# The $n%phase and&uadrature phase outputs are digiti'ed and pass through matched
lter and it is coherently integrated over inter pulse period
The resultant is nally sub ected to spectral moment estimation*we obtain parameters such as power* +oppler shift and spectralwidth
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Speci cations of MSTRadar : NARL !adan"i
5peratin" 0re'uency 1 .-M+, 6/+07Trans$itted po!er 1)3.M!
#ulse !idth 1 2 to -) $icro sec
Duty cycle 1 )3.8
Avera"e po!er 1 9 2* ; 4$ )
#ulse repetition 0re'uency 1 ?a"i%Uda antennas arran"ed in -) X -) s'uare "rid o&
*39@ spacin"
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Literature sur#e$ At$ospheric Layers +o! echoes received &ro$ At$ospheric Layers
Radar ran"e e'uations &or hard tar"et and distri(uted tar"ets
Ionospheric e ploration
Ran"e resolution #ulse co$pression
Radar receiver processin"
Matched &ilter
#o!erB Doppler and spectral !idth
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%ontinuous &a#e Radar
C, -".scillator
O'T
Tx Antenna
+etector MixerAM!
$ndicator
IN
-x Antenna
(istatic: Rt
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E$ploys continual RADAR trans$ission
Separate trans$it and receive antennas
Relies on the CD5##LER S+I0T
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Pulse Radar "requen Transm
!ulse wid
+uty
Average pow
!ulse repeti
PRT
P&
+Listening,Time
PRT*-.PR/
%arrier /re01
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S$nchroni2er Transmitter
Po3erSuppl$
Indicator Recei#er
Duple4er ANT1
Antenna Control
: c h o
$ n
- " . u t
Monostatic : R *%TR5
6+river*M.+*.;C
T
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Range The distance o& the tar"et can (e calculated &ro$ the
R 1 ct ) $eters
To tar"et short ran"e has to trans$it pulses !ith short duratios$all listen period 6>.** pulses per sec 7
0or lon" distancesB pulses !ith lar"e duration !ith $ore list period 6 F** pulses per sec 7
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Ma4imum 'nam8iguousRange The range corresponds to two%way time delay isknown as maximum unambiguous range
T 1 T 2 T 3 Tx
pulse
Rx echopulse
R2 1 c t )
t
Una$(i"uous ran"e
t
R) 1 c 6T t7 )
Echo 1 Echo 2
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Range Resolution
c T/4
c T/2
c T
c T c T
3 c T/2
R1 R2
R1 R2
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Pulse %ompression To increase the avera"e trans$itted po!er lon" pulse is used
It leads to de"rade in ran"e resolution
To overco$e this pro(le$ pulse co$pression is used
#ulse co$pression is achieved (y $odulatin" the pulse
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Pulse compression
Frequency Phase or Biphase
linear BarkerNon linear Complimentaryor Golays co de
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Linear /M
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Non 9 Linear /M
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%omparison of Linear and Nonlinear /M
L0M has $ore side lo(es
NL0M has less side lo(es
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t/7#73T ( Two Targets)
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t/7#730T
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t/7#710T
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t/7#73T (;>- %40d=)
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Tx signal
Pulse
coding
(ar"er %oding
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Barkercoderesponse
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t/7#30t (Two Targets)
t/7#0t
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t/7#0t
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t/7#60t
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t/t
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t/4#30t
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t/4#0t
/4#60
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t/4#60t
t/3t
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t/3t
t/7#30t (;> %40d=)
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t/7#30t (;>- %40d=)
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%omplimentar$ %oding Two length unimodular sequences x(t) and y(t) are
?olay complementary if the sum of theirautocorrelation functions satis es
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t/4#0t (Two Targets)
/4#60
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t/4#60t
t/3t
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t/3t
t/3#30t
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t/3#30t
t/4#0t (;> %34d=)
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t/4#0t (;>- %34d=)
% i f ( " d
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%omparison of (ar"er andcomplimentar$ code
Har=er code havin" sy$$etrical side lo(es
o$pli$entary codes totally eli$inates the side lo(es
4ea=er tar"ets also resolved in co$pli$entary
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References:23 CMiddle at$osphere pro"ra$ B hand (oo= &or $ap edited (y S3 0u=ao
)3 CA short history o& radar leadin" to at$ospheric pro&ilin" B H3H3HalsleyB IRESB University o&
-3 CRadar o(servation o& !inds and tur(ulence in the StratosphereB Mesosphere B Ronald 03 !ood$an aAl(erto GuillenB2F9>
>3 CSpectral $o$ent esti$ation in MST radars B Ronald3 03 4ood$anB 2F;.
.3 C+istorical Aspects of Radar At$ospheric Dyna$ics B (y S. Kato
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Than" ou