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Abstract. We present a new post-processing methodology for the analysis of InSAR (Synthetic Aperture Radar Interferometry) multi-temporal measures, based on the temporal under-sampling of displacement time series, the identification of potential changes occurring during the monitoring period and, eventually, the classification of different deformation behaviours. The potentials of this approach for the analysis of geological processes were tested on the case study of Naro (Italy), specifically selected due to its geological setting and related ground instability of unknown causes that occurred in February 2005. The time series analysis of past (ERS1/2 descending data; 1992–2000) and current (RADARSAT-1 ascending data; 2003–2007) ground movements highlighted significant displacement rates (up to 6 mm yr−1) in 2003–2007, followed by a post-event stabilization. The deformational behaviours of instable areas involved in the 2005 event were also detected, clarifying typology and kinematics of ground instability. The urban sectors affected and unaffected by the event were finally mapped, consequently re-defining and enlarging the influenced area previously detected by field observations. Through the integration of InSAR data and conventional field surveys (i.e. geological, geomorphologic and geostructural campaigns), the causes of instability were finally attributed to tectonics.
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Francesca Cigna
Institute of Atmospheric Sciences and Climate
Chiara Del Ventisette
Institute of Geosciences and Earth Resources
Vincenzo Liguori
NOAA Oceanic and Atmospheric Research
Natural hazards and earth system sciences
University of Florence
University of Palermo
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Cigna et al. (Wed,) studied this question.
synapsesocial.com/papers/6a1bf8e9b33628da419d10b7 — DOI: https://doi.org/10.5194/nhess-11-865-2011