Abstract
The need of living together with landslides in a sustainable way requires a strong effort in terms of landslide analysis. Traditional methods used for mapping and monitoring mass movements can benefit from the application of remote sensing techniques coupled with GIS analysis. The use of remote sensing technologies, whether air, satellite or ground based allows a rapid acquisition of quantitative data over wide areas, reducing the field work and, as a consequence, the costs. A modern satellite radar interferometry method of Permanent scatters (PSInSAR) is very useful. At Geological Survey of Slovenia, the PSInSARTM data were used to assess spatio-temporal factors which influence on slope mass movements and small, long lasting ground deformations were defined in the Škofjeloško Cerkljansko area during the years 1992–2000.
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Buser S (1987) Osnovna geološka karta SFRJ, list Tolmin in Videm, 1: 100,000 = basic geological map of Yugoslavia, Tolmin and Udine, scale 1: 100,000. Zvezni geološki zavod, Belgrade
Cascini C, Fornaro G, Peduto D (2009) Analysis at medium scale of low resolution DInSAR data in slow moving landslide affected areas. ISPRS J Photogramm Rem Sens 64(6):598–611
Colesanti C, Ferretti A, Novali F, Prati C, Rocca F (2003) SAR monitoring of progressive and seasonal ground deformation using the Permanent Scatterers Techniques. IEEE Trans Geosci Rem Sens 41(7):1685–1701
Farina SD, Colombo A, Fumagalli F, Marks S, Moretti S (2006) Permanent Scatterers for landslide investigations: outcomes from the ESA-SLAM project. Eng Geol 88:200–217
Ferretti A, Prati C, Rocca F (1999) Non-uniform motion monitoring using the permanent scatterers technique. In: Second international workshop on ERS SAR interferometry
Ferretti A, Prati C, Rocca F (2001) Permanent scatterers in SAR interferometry. IEEE Trans Geosci Rem Sens 39(1):8–20
Grad K, Ferjančič L (1974) Osnovna geološka karta SFRJ, list Kranj, 1: 100,000 = basic geological map of Yugoslavia, Map Kranj, scale 1: 100,000. Zvezni geološki zavod, Belgrade
Milone G, Scepi G (2011) A clustering approach for studying ground deformation trends in Campania region through PS-InSARTM time series analysis. J Appl Sci 11:610–620
Placer L (1999) Contribution to the macrotectonic subdivision of the border region between Southern Alps and External Dinarides. Geologija 41:223–255, Ljubljana
Placer L, Rajver D, Trajanova M, Ogorelec B, Skabarne D, Mlakar I (2000) Borehole Ce-2795 at Cerkno at the boundary between the Southeren Alps and the External Dinarides (Slovenia). Geologija 43(2):251–266, Ljubljana
Acknowledgments
The authors would like to thank the Research Agency of the Republic of Slovenia (ARRS) for funding the research (J1-0913) and JTS of Alpine Space-European Territorial cooperation programme for co-funding the research through the AdaptAlp project.
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Auflič, M.J., Čarman, M., Komac, M. (2013). Assessing of Spatio-Temporal Factors Influencing Landslides Using PSInSAR. In: Margottini, C., Canuti, P., Sassa, K. (eds) Landslide Science and Practice. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-31445-2_48
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DOI: https://doi.org/10.1007/978-3-642-31445-2_48
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