Persistent Scatterers continuous streaming for landslide monitoring and mapping: the case of the Tuscany region (Italy)

The results of the continuous monitoring of ground deformation throughout the Tuscany region using radar images acquired by the Sentinel-1 satellite constellation of the European Space Agency (ESA) are presented here. This new monitoring approach, based on systematic imagery processing and analysis...

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Veröffentlicht in:Landslides 2019-10, Vol.16 (10), p.2033-2044
Hauptverfasser: Raspini, Federico, Bianchini, Silvia, Ciampalini, Andrea, Del Soldato, Matteo, Montalti, Roberto, Solari, Lorenzo, Tofani, Veronica, Casagli, Nicola
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Sprache:eng
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Zusammenfassung:The results of the continuous monitoring of ground deformation throughout the Tuscany region using radar images acquired by the Sentinel-1 satellite constellation of the European Space Agency (ESA) are presented here. This new monitoring approach, based on systematic imagery processing and analysis of deformation time series, is discussed at regional (for the entire Tuscany) and at local scale in the context of a case study of the Carpineta landslide, which is a large, active earth slide in the Northern Apennines (Pistoia province). The landslide registered an acceleration during the winter and spring of 2018 as a direct consequence of rainfall and snow melt. The increase in the deformation rate of the landslide, which led to the damage of several buildings, was promptly detected and monitored due to the enhanced temporal repetitiveness offered by the Sentinel-1 constellation. The results demonstrate that advances in satellite sensors, increases in computing capacity and the refinement of processing approaches and data screening tools can contribute to the development of new paradigms in satellite-based monitoring systems. Sentinel-1 data, which are systematically acquired with short revisiting times and then promptly processed, can now be used as a tool for the systematic tracking of ground deformation at the regional scale and for the continuous monitoring of slow and very slow landslides.
ISSN:1612-510X
1612-5118
DOI:10.1007/s10346-019-01249-w