introduction to sar interferometry

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Introduction to SAR interferometry Rüdiger Gens

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Page 1: Introduction to SAR interferometry

Introduction to SAR interferometry

Rüdiger Gens

Page 2: Introduction to SAR interferometry

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Outline

! Relevant terms! Geometry! Why does InSAR work?! Techniques! Products! Applications! Error sources! Trends and challenges

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Relevant terms

! amplitude" measure of the

strength of the signal ! phase

" angle of a complex number

Page 4: Introduction to SAR interferometry

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Relevant terms

! baseline" separation between the two antenna positions either

mounted on an aircraft or realized by two repeating satellite orbits

Source: Gens and van Genderen, IJRS, 1996

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Relevant terms

! fringe" represents the whole

range of the phase in an interferogram from 0 to 2π in a full colour cycle

Page 6: Introduction to SAR interferometry

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Geometry of SAR interferometry

z

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Why does InSAR work?

! coherent signal" single frequency

! same geometry covering the same area from slightly different position in space

Does optical interferometry work?

! coherent light source: ! application: holography

laser

yes

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Interferometric techniques

! across-track interferometry" regular airborne geometry

! along-track interferometry" airborne geometry" monitoring ocean currents or other moving objects

! repeat-pass interferometry" usually spaceborne

! differential interferometry" change detection

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Across-track interferometry

! presently only employed on airborne system

! two SAR antenna systems to be mounted simultaneously on the platform perpendicular to the flight direction

! distinction between errors caused by the aircraft roll and the influence of the terrain slope is not possible.

hx

r2

r1

z r21

θ21

θlook

H

flight path

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Along-track interferometry

! only applicable to airborne SAR systems

! yaw and pitch cause baseline components in y- and z-direction which produce additional phase differences.

! calibration of the phase difference is necessary before absolute velocity measurements are possible

x

hy

r2

r1

z r21

θ21

θlook

H

flight path

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Repeat-pass interferometry

! requires only one antenna

! most suited to spaceborne sensors

! precise location of the flight path is required

! satellite passing nearly the same orbit to cover an area twice with a slightly different viewing geometry.

flight pathsz O2

O1

r2

r1

h

yx

H

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Interferogram

complex multiplication of the two images; i.e. the correspondingamplitudes have to be averaged and the corresponding phases have to be differenced at each point in the image

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Coherence image

"measure for the correlation of corresponding signals"ranges from 0 to 1

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Digital elevation model

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Digital elevation model

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Differential interferogram

! change detection: measurement of small-scale movements in the vertical direction

! displacement measured is not vertical, but along the viewing direction

! relative accuracy of the order of a few centimetres or even less vs. absolute accuracy of digital elevation models of about 10-15 meters (for ERS data)

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Interferometric applications

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Seismic events

Source: Massonnet et al. (1993)

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Volcanic hazards

Source: Massonnet (1997)

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Glacier research

Image Credits:Received by CCRSPre-processed by RSI

Interpretation:Laurence Gray, CCRSKarim Mattar, IntermapParis Vachon, CCRS

© CSA, 1996

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Land subsidence

Source: http://www.gamma-rs.ch/research/mexico.html

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Forestry

Source: Strozzi and Wegmüller (1997)

interferometric correlation

backscatter intensity

backscatter change

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Error sources

! atmospheric effects" maybe most limiting factor for differential InSAR" delays signal return" can be heterogeneous and very local

→ difficult to determine" change the tropospheric water vapor content" new research field for studying of tropospheric

turbulences and ionospheric phenomena

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Error sources

! orbits" predicted vs. restituted vs. precise orbits

! temporal decorrelation" caused by physical changes in the surface over the

time period between observations

! baseline decorrelation" higher noise level with increasing length of baseline

→ decorrelation of radar signal

! processing

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Trends and challenges

! Shuttle Radar Topography Mission (SRTM)" flown in February 2000

! swath processing" data volume" Doppler frequency issues

! DEM production for larger areas" SRTM" AKDEM project

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Questions