Articles | Volume 13, issue 7
https://doi.org/10.5194/nhess-13-1873-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/nhess-13-1873-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
29 Jul 2013
Research article |
| 29 Jul 2013
Non-interferometric GB-SAR measurement: application to the Vallcebre landslide (eastern Pyrenees, Spain)
O. Monserrat
Institute of Geomatics, Castelldefels, Barcelona, Spain
J. Moya
Dept. of Geotechnical Engineering and Geosciences, Technical University of Catalonia-BarcelonaTech, Barcelona, Spain
G. Luzi
Institute of Geomatics, Castelldefels, Barcelona, Spain
M. Crosetto
Institute of Geomatics, Castelldefels, Barcelona, Spain
J. A. Gili
Dept. of Geotechnical Engineering and Geosciences, Technical University of Catalonia-BarcelonaTech, Barcelona, Spain
J. Corominas
Dept. of Geotechnical Engineering and Geosciences, Technical University of Catalonia-BarcelonaTech, Barcelona, Spain
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Manuscript not accepted for further review
Short summary
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In this work, the Cross-Correlation Function is used in order to quantitatively investigate the time-lagged correlation between high frequency monitoring data on rainfall, piezometric and displacement with the objective to evidence hydro-mechanical processes in the Vallcebre landslide (Eastern Pyrenees, Spain). The analysis highlighted and constrained in time a dual triggering mechanism in which factors controlling movement change from the upper to the lower part of the landslide.
M. Crosetto, O. Monserrat, N. Devanthéry, M. Cuevas-González, A. Barra, and B. Crippa
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M. Crosetto, N. Devanthéry, M. Cuevas-González, O. Monserrat, and B. Crippa
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Short summary
Persistent Scatterer Interferometry (PSI) is a remote sensing technique used to monitor land deformation from interferometric SAR images. The main products that can be derived using the PSI technique are the deformation maps and the time series of deformation. In this paper, an approach to apply the PSI technique to a stack of Sentinel-1 images is described. Sentinel-1 deformation maps and time series obtained over the metropolitan area of Mexico DF are discussed.
C. Abancó, M. Hürlimann, and J. Moya
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M. Crosetto, J. A. Gili, O. Monserrat, M. Cuevas-González, J. Corominas, and D. Serral
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