ESA Earth Home Missions Data Products Resources Applications
    15-Feb-2012
EO Data Access
How to Apply
How to Access
Radar Course III
43. Texture and image analysis
42. Temporal averaging
12. Synthetic Aperture Radar (SAR)
34. Space, time and processing constraints
15. Slant range / ground range
8. Side-looking radars
19. Shadow
10. Real Aperture Radar: Range resolution
11. Real Aperture Radar: Azimuth resolution
9. Real Aperture Radar (RAR)
7. Radar principles
38. Radar image interpretation
35. The radar equation
36. Parameters affecting radar backscatter
16. Optical vs. microwave image geometry
25. Method
18. Layover
32. Landers Earthquake in South California
23. Introduction
27. Interferogramme of Naples (Italy)
29. Interferogramme and DEM of Gennargentu (Italy)
2. Independence of clouds coverage
40. Image interpretation: Speckle
41. Image interpretation: Speckle filters
39. Image interpretation: Tone
20. Geometric effects for image interpretation
22. Geocoding: Geometry
17. Foreshortening
26. First ERS-1/ERS-2 tandem interferogramme
6. Electromagnetic spectrum
30. Differential interferometry
45. Data reduction: 16 to 8 bit, blockaverage vs incrementing
4. Control of imaging geometry
3. Control of emitted electromagnetic radiation
24. Concept
28. Coherence image of Bonn area (Germany)
44. Classification of ERS-1 SAR images with Neural Networks
37. Bragg scattering
5. Access to different parameters compared to optical systems
13. SAR processing
33. SAR interferometric products
21. SAR image geocoding
14. ERS SAR geometric configuration
31. The Bonn experiment
Services
Site Map
Frequently asked questions
Glossary
Credits
Terms of use
Contact us
Search


 
 
 

SAR interferometric products

ERS-1 quarter-scenes are presented as (raw) input, intermediate and possible final interferometric products. ESA currently offers no interferometric
products beyond the basic SLC full or quarter-scene image.
The essential difference when compared to conventional detected SAR products (e.g. PRI) is that the phase resulting from the backscattered pulses of a target is preserved and used. Interferometric data applications use the phase change between acquisitions from the same orbital track. In principle, a minimum of one pair of data sets is necessary. Data application includes coherence maps, digital elevation models and mapping of small (centimeter-range) Earth movements.
The images presented in the following show parts of the Swiss Plateau crossed by the Aare river east to west.
In the examples below radar illumination is from the right and the flight direction is approximately north-south (descending pass). The data was acquired
on November 24 and 27, 1991.

SERIES OF IMAGES:
Raw Data
Range compressed Data
One Look Complex Image
One Look Complex Detected Image (I)
One Look Complex Detected Image (II)
Raw Interferogramme
Interferogramme
Coherence Image
Digital Elevation Model

SERIES OF IMAGES (continuous display):

All image processing and text by: D. Small, E. Meier, D. Nuesch Remote Sensing Laboratories, Dept. of Geography, University of ZurichGeography, University of Zurich

Keywords: ESA European Space Agency - Agence spatiale europeenne, observation de la terre, earth observation, satellite remote sensing, teledetection, geophysique, altimetrie, radar, chimique atmospherique, geophysics, altimetry, radar, atmospheric chemistry