EGU25-11254, updated on 15 Mar 2025
https://doi.org/10.5194/egusphere-egu25-11254
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Tuesday, 29 Apr, 16:55–17:05 (CEST)
 
Room 1.15/16
Dynamics of slow-moving landslides in the Eastern Cordillera of the Central Andes derived from optical satellite imagery
Florian Leder, Ariane Mueting, Aljoscha Rheinwalt, and Bodo Bookhagen
Florian Leder et al.
  • Institute of Geosciences, University of Potsdam, Potsdam-Golm, Germany

The Eastern Cordillera of the Central Andes in Northwestern Argentina and Southern Bolivia is an actively deforming mountain front with elevations ranging from ~1 km in the foreland to ~4 km and higher on the Central Andean Plateau. The orographic barrier induces a strong climatic and environmental east-west gradient with peak rainfall in the steep eastward-facing slopes. Frequent rainstorms during the South American summer monsoon in combination with fault-weakened lithologies drive mass-movement processes. The resulting debris flows and landslides pose a serious threat to the local infrastructure.

In this study, we integrate satellite-based optical remote sensing data over the last 10 years to characterize the long-term dynamics of slow-moving landslides in the eastern Central Andes in Argentina. In this way, we aim to establish potential relationships between climatic seasonality, seismic activity and landslide deformation signals. We apply a combination of pixel and feature-based tracking approaches to a data set comprising a network of medium-resolution Sentinel-2 and Landsat 8, and high-resolution SPOT7 optical images. The final ground displacement time series in east-west and north-south directions were reconstructed through time-series inversion. Vertical variations were obtained by comparing high-resolution Digital Surface Models (DSM) produced from tri-stereo SPOT7 images. We attempt to improve the detection of very slow-moving landslides with velocities below 0.5 m/yr by stacking multiple matching pairs and relying on feature-based tracking approaches. In some examples, the displacement time series reveal metric ground displacements following earthquake events observed in the region, changing the dynamics of the landslide.

This study emphasizes the usefulness of large-scale, decadal-long time series of optical satellite imagery and presents a novel GPU-based approach of combining computer vision feature tracking methods with classic correlation based block matching.

How to cite: Leder, F., Mueting, A., Rheinwalt, A., and Bookhagen, B.: Dynamics of slow-moving landslides in the Eastern Cordillera of the Central Andes derived from optical satellite imagery, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-11254, https://doi.org/10.5194/egusphere-egu25-11254, 2025.