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Map and Monitoring Slow Ground Deformation in NW Italy Using PSI Techniques

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Engineering Geology for Society and Territory - Volume 5

Abstract

This work describes the potentiality of Persistent Scatterers Interferometry (PSI) techniques into mapping, monitoring and characterizing some pattern of deformations related to different slow geological processes: landslides, subsidence, periglacial activity and other processes related to natural or anthropic causes. The study area is located in the NW Italy (>20,000 km2). Radarsat Canadian satellite (2003–2010) and European Remote-Sensing Satellite (ERS) satellite data (1992–2000) processed with advanced algorithm (SqueeSAR™) were used. Some representative case histories are here presented.

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Correspondence to Davide Notti .

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Notti, D., Meisina, C., Zucca, F., Colombo, A., Paro, L. (2015). Map and Monitoring Slow Ground Deformation in NW Italy Using PSI Techniques. In: Lollino, G., Manconi, A., Guzzetti, F., Culshaw, M., Bobrowsky, P., Luino, F. (eds) Engineering Geology for Society and Territory - Volume 5. Springer, Cham. https://doi.org/10.1007/978-3-319-09048-1_28

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