Active landslides deformations mapping and monitoring in rural areas using satellite radar interferometry
<p>Landslide hazards pose as one of the greatest risks in today&#8217;s context of climate change and settlement expansion. The later process occurs both in the urban and rural areas and significantly changes the terrain morphology and contributes as a conditioning factor for the triggering of new landslide events or reactivation of old dormant ones. Usually, the urban areas are of a greater interest to assess the activity of landslides and their associated risks. On the other hand, the remote areas such as the rural settlements are not as much investigated and monitored, mostly because the in-situ investigations requires additional costs for the deployment of various instruments.</p><p>In the last decades, the development of Advanced Differential SAR Interferometry techniques permits to identify and monitor these geomorphological processes from space. They rely on the microwave&#8217;s signal properties to quantify with millimeter accuracy possible deformations in time. The advances of satellite&#8217;s acquisition capabilities and the increase of computational power allow the mapping of active landslides over wide areas and even detection of failure precursors.</p><p>In our case, we used the DInSAR techniques to identify the active landslides over a large area in the Moldavian Plateau that affects the human settlements. Even though for the urban areas was much easier to detect the landslide induced deformations, in the case of the rural communities this task was much more challenging. We used the COMET-LiCS Sentinel-1 InSAR data (LiCSAR) and the LiCSBAS software for processing the data for the Moldavian Plateau, Northeastern Romania. Based on the results post-processing we classified the landslides activity based on their velocity and we created an active landslide inventory of the area.</p>