1. InSAR and LIDAR
Lecture 8
Oct 13, 2004

2. Interferogram of Landers earthquake 7. 3 magnitude on June 18, 1992
Interferogram of Landers earthquake 7.3 magnitude on June 18, This is a remarkable new tech gained recognition thereafter.
This is from ERS-1
Average displacement along the fault rupture was 3-4 m, maximum was 6m.
Each color cycle represents additional 2.8 cm ground motion or displacement.

3. Interferometric Synthetic aperture radar (InSAR)
Elevation
Surface Displacement

4. Principals One SAR with 2 antennas (single-pass)
AIRSAR/TOPSAR
Along track interferometric mode (ATI) (L and C)
Ocean current and waves
Cross track interferometric mode (TXI) (L or C)
DEM (3-5 m or 1 m)
Shutter Radar Topographic Mission (SRTM)
C band and X band antennas separated by 60 m
One SAR in different times (multi-pass)
SIR-C
ERS 1,2

9. Calculate altitude (1) (2) (3) (4)
 is the fractional phase (value 0-2 radians)

13. Glaciers are sensitive indicators of climatic change
Glaciers are sensitive indicators of climatic change. They can grow and thicken with increasing snowfall and/or decreased melting. Conversely, they can retreat and thin if snowfall decreases and/or atmospheric temperatures rise and cause increased melting. Landsat imaging has been an excellent tool for mapping the changing geographic extent of glaciers since The elevation measurements taken by SRTM in February 2000 now provide a near-global baseline against which future non-polar region glacial thinning or thickening can be assessed.

15. Source for SRTM data USGS gallery: JPL gallery:
USGS seamless distribution system

16. SRTM coverage map
To download from here

17. Surface Displacement
Ferretti et al. 2004

18. There is a new method called Permanent Scatterer (PS)
Can determine mm-scale displacements of individidual
Features. More than 15 acquisitions needed for calculation
GPS has difficulty
to resolve mm./y

19. LIDAR
LIght Detection And Ranging uses the same principle as RADAR. The lidar instrument transmits laser out to a target. The transmitted light interacts with atmosphere and target. Some of this light is reflected / scattered back to the instrument where it is analyzed.
Use UV, visible, and infrared
Transmitter (laser), receiver, and detector
Distance = C x T /2
Four types
Ranger finders: it is the simplest lidars, it measures the distance, then create the topographic map
DIAL: Differential Absorption Lidar is used to measure chemical concentrations (such as ozone, water vapor, pollutants) in the atmosphere.
Doppler Lidars: it’s used to measure the velocity of a target
Raman LIDAR: can measure gaseous species

20. Airborne Lidar System ALTMS (TerraPoint, USA)
FLI-MAP (John Chance, USA)
ALTM (USA)
TopoEye (USA)
ATLAS (USA)

21. Lidar elevation data of Bristol, UK

22. These data are collected with aircraft-mounted lasers capable of recording elevation measurements at a rate of 2,000 to 5,000 pulses per second and have a vertical precision of 15 centimeters (6 inches). After a baseline data set has been created, follow-up flights can be used to detect shoreline changes.

23. Surface and DTM

24. DSM and DTM
DTM (bare)
DSM

25. Airborne Lidar

26. DIAL laser measures water vapor, clouds, and aerosols by comparing the absorption and scattering of different laser pulses on these atmospheric species

27. CALIPSO
Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations, to be launched 2005.
Will provide a global set of data on aerosol and cloud properties, radiative fluxes, and atmospheric state.
Equipment:
Lidar: 632 nm and 1064 nm
Radiometer
Camera

28. Calipso instrument

29. Midterm review