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UAF Class GEOS 657
GEOS 657 – MICROWAVE REMOTE SENSINGSPRING 2019
Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks; [email protected]
Lecture 7: Principles of Radar & Active Microwave Systems
Image: DLR, CC-BY 3.0
Franz J Meyer, UAF
GEOS 657: Microwave RS - 2
Sentinel-1 C-band Radar monitors Dam Break in Brazil
Before dam breach: 2019-01-22
Recent “Radar in the News”
Franz J Meyer, UAF
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Sentinel-1 C-band Radar monitors Dam Break in Brazil
Before dam breach: 2019-01-22After dam breach: 2019-01-28
Recent “Radar in the News”
Franz J Meyer, UAF
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VS.2019-01-22
2019-01-28
Recent “Radar in the News”Se
nti
nel
-1 S
AR
O
ptical2019-01-29
2019-01-24
Planet Labs
Planet Labs
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• Some Basics and Three Types of Radar Systems
• Imaging Radars - Concepts:
– The Radar Equation
– Separating Several Range Resolution Cells within Antenna Footprint
• Imaging Radars – How it’s Really Done:
– The Concept of Pulse Compression Systems
– The Resolution-Bandwidth Duality
– Range Compression – The Matched Filter Approach
• Examples of Imaging Radar Data
Outline
5
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SOME BASICS AND THREE TYPES OF RADAR SYSTEMS
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Active Microwave Systems are called RADARs
• Radars actively transmit microwave signals (usually a radar pulse)
• Radar antenna provides directivity for transmitted signal
• A radar sensor records three different parameters: Amplitude, Phase and polarization of the reflected microwave signals (here we focus on amplitude and phase)
Detected amplitude measures surface radar cross section (RCS)
Timing of transmitted signal (radar pulse) provides information about distance between
satellite and ground
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Three Different Types of Radar Systems
• Based on measurement type, three different radar systems can be discriminated:
Non-Imaging Systems
RADAR ALTIMETERS
Measuring distance
(from travel time)
Trans-
mitted
pulses
SCATTEROMETERS
Measuring radar cross
section
Trans-
mitted
pulses
Imaging Systems
Range pixel
size ~ pulse
length
Azimuth
pixel size =
antenna
footprint (or
better when
doing SAR)
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Radar Principle
TX
RX
R
scattering
object
range
transmit
cR2
received echo:
(time)
light velocity
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• Radar altimeter emits pulses towards the Earth's surface (nadir direction)
• Signal travel time (transmission to reception) is proportional to satellite altitude.
A Short Word on Radar Altimeters
10
• Measuring Signal travel time not easy as echo signal has funny shape
Idealized altimeter echo from flat surface (e.g., smooth ocean surface
Reference EllipsoidGeoid Undulations
Dynamic Topography
Barometric EffectTides SWH
Center of Mass
Instantaneous Sea Level
Orbit Height = H
Mean Sea Level = SSHmean
Geoid = Hgeoid
Sensor Geometry
Ionosphere
Dry Troposphere
Wet TroposphereHmeasured
11
Calculating Surface Height from Altimeter Measurements
Mean Sea Level Height from AltimetryM
ean
Sea
Lev
el M
arch
20
06
12
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Microwave Scatterometers
• Goal: measurement of wind speed and direction over oceans
wind
ocean
surface
roughness
radar
backscatter
Example: Scatterometer on ERS
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QuikSCAT Windfield
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IMAGING RADAR CONCEPTS
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The Radar Equation – A Reminder
transmit power: WPt
224 m
W
R
GPt
power density at scatterer:
antenna gain:2
4
AG
radar cross section: 2m
WR
GPt 24
reflected power:
antenna area: 2mA
received power:
WR
GP
R
GPG
R
GPAP t
ttr
43
22
42
2
424444
242
4 m
W
R
GPt
power density at receiver:
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Pulse Waveform and Range Resolution
targets #1 and #2 easily separable, if 2cPRR (range resolution)
transmit
receive
PR R
targets:
#1 #2
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Range Resolution Example
• Insufficient Target Separation
• Sufficient Target Separation
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AN A BIT MORE ESOTERIC THINK – PAIR –SHARE
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1. Explain what the “Spectrum (Fourier Representation)” of an Image represents
2. Assign the right spectrum to the right image:
3. Based on these image relationships above, which image parameter dictates how “wide” the spectrum of the image is?
Think – Pair – ShareWhat does the Spectrum of an Image Tell Us?
Image #1 Image #2 Image #3
Spectrum #A Spectrum #B Spectrum #C
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IMAGING RADAR – HOW IT’S REALLY DONE
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Some Problems with the Radar Imaging Concept
• Power 𝑷𝒓 of returned signal reduces rapidly the distance 𝑹 to the target
𝑃𝑟 ∝1
𝑅4𝑃𝑡 𝑤𝑖𝑡ℎ 𝑃𝑡 = 𝑡𝑟𝑎𝑛𝑠𝑚𝑖𝑡 𝑝𝑜𝑤𝑒𝑟
• For satellite applications: 𝑃𝑟 ≈1
400000000000000000000000∙ 𝑃𝑡!!!!!!!
For Satellite applications:Difficult to transmit a pulse that (1) has enough power to be able to detect backscattered response AND (2) is short enough to yield sufficient range resolution
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Most Radars Replace Pulse with Linear Frequency Modulated (Chirped) Signal
• Reason: Sending sufficient power in a single short pulse is near impossible
• Radars that send chirped signal are called “Pulse Compression Systems”
• Procedure:
1. Transmit frequency coded signal of length 𝜏𝑃2. Receive frequency coded echo
3. Compress frequency coded signal using a decoding operation called matched filtering
• What is the resolution of the compressed pulse?
– Ability to compress the pulse depends on the bandwidth 𝑊𝑃 of transmitted chirp signal
– The higher the bandwidth, the narrower the compressed pulse
→ 𝜏𝑃 =1
𝑊𝑃
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Achieving Good Range ResolutionThe Airborne Case
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Achieving Good Range Resolution The Spaceborne Case
transmitted signal echo of pulses
Use a focusing process to recover the smeared targets
Send a longer “chirped” signal to increase 𝑃𝑡
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Properties of the Frequency Coded (Chirped) Signal
• Chirp signal: 𝑢 𝜏 = 𝑒𝑥𝑝 𝑗𝜋𝑘𝜏2 = 𝑐𝑜𝑠 𝜋𝑘𝜏2 + 𝑗 ∙ 𝑠𝑖𝑛 𝜋𝑘𝜏2
Frequency 𝑓
Radar center frequency 𝑓0
Chirp rate 𝑘
Pchirp pulse duration:
Time 𝜏
Time 𝜏
Band
wid
th 𝑊
𝑃
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1. Data Acquisition:
Shape of compressed pulse
Range Compression by Matched Filtering (I)
logarithmic
-10 dB
-20 dB
resolutionlinear (magnitude) sinc
resolution
Side lobes
1. Transmit chirp instead of short pulse
2. Every point target will return chirp echo
3. Final range resolution after Range Compression: 𝜌𝑅 ≅𝑐
2𝑊𝑃
2. Range Compression:Correlate received signal with replica of
transmitted chirp
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Range Compression by Matched Filtering (II)
correlation
R
Focused pulse
reference chirp
signal
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Range Compression: Resolution-Bandwidth Duality
• You see two different chirps of identical duration but different chirp rates (𝑘 = 50 & 𝑘 =100 Hz/s)
• Higher chirp rate twice the bandwidth two times better resolution after correlation
Chirp BandwidthChirp in time domain
k =
10
0 H
z/s
k
= 5
0 H
z/s
Correlation Result
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Range Compression: Matlab Example (I)
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Range Compression: Matlab Example (II)
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Range Compression: Matlab Example (III)
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Chirp-Rate Error Effects – Matlab Example
𝑘𝑠: Chirp rate of
transmitted signal
𝑘𝑓: Chirp rate used
for focusing
Chirp rate errors
→ insufficient
focusing of
scattered energy
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Where Do Side-Lobes Come From?Effect of Windowing – Matlab Example (I)
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Where Do Side-Lobes Come From?Effect of Windowing – Matlab Example (II)
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EXAMPLES OF IMAGING RADAR DATA
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Side-Looking Airborne Radars (SLARs)
• Developed in 1950s driven by military
• Key element: Long antenna transmitting narrow fan-beams sideways from the aircraft
• Resolution defined by pulse length & length of antenna
• Resolution generally fair
Side-Looking Radars Use Pulse Compression to Increase Range Resolution
Flight direction
Pixel in a SLAR image
Pulse footprint
= along-track resolution
Pulse length = range resolution
Principle of a SLAR System
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Imaged (scanned)
area
Scanning Ground-based Radar System as a SLAR Example
• Resolution defined by pulse length & length of antenna
Imaging the Surface with SLARs
Radial decrease in
resolution
scan
direction
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Example of Scanning Ground-Based Radar Acquisition
• 180 degrees scan angle – location: Fairbanks, Alaska
Sensor Location
Decre
asin
g r
eso
lution (
in s
ca
n
dire
ctio
n)
with
ran
ge
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What’s Next?
• After improving resolution in range we also want to enhance the azimuth resolution of imaging radars
• Hence, next lecture (Tuesday 20-Feb-17) we will chat about something called “Aperture Synthesis” (the basis of Synthetic Aperture Radar)
• In preparation please read in Woodhouse (2006):
– Pages 271 – 280
– Specifically think about the two different interpretations of the aperture synthesis process (we will discuss those in class)