
doi: 10.5772/34224
handle: 20.500.14243/9956
Differential Synthetic Aperture Radar Interferometry (DInSAR) represents nowadays a wellestablished remote sensing technique to generate spatially dense surface deformation maps of large areas on Earth (Massonnet & Feigl, 1999; Burgmann et. al., 2000). To achieve this task, the phase difference (known as interferogram) between SAR data pairs related to temporally-separated observations is exploited, retrieving a measure of the ground displacement projection along the radar line of sight (LOS) with centimeter to millimeter accuracy (Gabriel et. al., 1989).
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