L'interferometria SAR satellitare per la misura delle deformazioni superficiali

Abstract

La tecnica interferometrica, basata  sull'elaborazione coerente della fase del ritorno del segnale radar dalla superficie terrestre, ha reso il telerilevamento radar uno strumento di analisi quantitativa in molteplici campi applicativi quali cartografia, geodesia, rischio sismico, idrogeologico e vulcanico. In particolare, l'InSAR consente di produrre mappe di spostamento co-sismico, ovvero di misurare  il campo di deformazione superficiale causato da un terremoto con accuratezze centimetriche.

Satellite  SAR  interferometry  for the measurement of surface deformation

The SAR Interferometry (InSAR) technique is mostly used to measure the characteristics of the topography and its  changes  during  time.  The  interferometric  technique,  based  on  the coherent elaboration of radar returns from the surface, has made the radar remote  sensing  a  valuable  tool  for a  quantitative  analysis  in  many  applicative  fields  such  as  cartography, geodesy, seismic, hydrogeologic and volcanic  hazards.  In  particular,  InSAR technique is able to measure the co-seismic  surface  deformation  caused by  an  earthquake  with  accuracies  at order of centimeters. This kind of data is extremely important for the estima-tion  of  the  geometric  parameters  of the seismic source  which is a relevant information  for  the  management  of event scenarios.In the last decade a new technique for the elaboration of the interferometric signal  arises,  the  multitemporal  SAR Interferometry. Thanks to the exploita-tion of a conspicuous number of SAR images,  it  is  possible  detecting  and monitoring the slow soil deformation with millimetric accuracies. Moreover, the recent very high resolution satellite  SAR  sensors  make  possible  to apply  this  technique  in  urban  areas in  order  to  monitor  single  structures such as bridges, buildings, roads and so on.