ESA Earth Home Missions Data Products Resources Applications
    16-May-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


 
 
 

Concept

Interferometry allows the measurement of high resolution topographic profiles of terrain from multiple-pass SAR data sets. For the interferometric technique to be applicable, these data sets must be obtained when the sensor is in repeat orbit, such that the scene is viewed from almost the same aspect angle for each of the passes.

The figure shows the interferometric imaging geometry pointing out the two passes with range vectors r1 and r2 to the resolution element. The look angle of the radar is , the baseline B is tilted at an angle measured relative to horizontal.

Each pixel of a SAR image contains information on both the intensity and phase of the received signal. The pixel intensity is related to the radar scattering properties of the surface, and the pixel phase to the satellite to ground path length, or distance.

Intensity images are the form of SAR data that is most frequently presented and probably most familiar to the public.
However, it is the phase information only (and not the image intensity) that is exploited by interferometric techniques, it contains informations about heights orthogonal to the SAR image plane.

An interferometer is a device that superimposes or mixes wave phenomena from two coherent sources.
First, the two SAR images are registered to each other to identify pixels corresponding to the same area of the Earth's surface.

Then, for each pixel, the phase values are subtracted to produce the phase difference image known as an interferogramme. This phase difference is a
measure of the difference in path length from a given pixel to each antenna of the SAR interferometer.

The resulting interference effects are well-known both in optics (e.g., Newton's rings formed when a convex lens is placed on a plane surface) and sonics (e.g., beating formed by two similar frequency sound waves). Radar interferometry is the analogous phenomenon in the microwave region of the electromagnetic spectrum.

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