PSI is a powerful
remote sensing technique able to measure and monitor displacements of the Earth's surface over time with the highest possible accuracy of displacement estimation (2–4 mm in height). Input data should include at least 20-25 images of the same territory with different dates, made in the same geometry of the satellite radar survey.
Algorithm:
1. Selecting the original image
2. Co-registration of interferometric circuit pulses with an accuracy of 1/100 of a pixel
3. Building an interferogram for each pair of images
4. Estimation of the magnitude of coherence / standard deviations of the amplitude of each pair of measurements
5. Determination of points - stable scatterers of the radar signal
6. Evaluation of frequency differences and multi-time phase sweep for point targets by points, earlier
7. Application of an individual filter that removes the effect on the interferometric phase The result of processing is a vector file of points with:
- offsets for each shooting date;
- average annual rate of displacement;
- the total value of the displacements;
- height above the WGS-84 ellipsoid.