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Julien Travelletti

Researcher at University of Strasbourg

Publications -  19
Citations -  1206

Julien Travelletti is an academic researcher from University of Strasbourg. The author has contributed to research in topics: Landslide & Displacement (vector). The author has an hindex of 12, co-authored 18 publications receiving 1037 citations. Previous affiliations of Julien Travelletti include University of Lausanne & Ecole et Observatoire des Sciences de la Terre.

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UAV-based remote sensing of the Super-Sauze landslide : evaluation and results.

TL;DR: In this paper, a radio-controlled mini quad-rotor UAV of the Super-Sauze, France landslide has been used to produce a high-resolution ortho-mosaic of the entire landslide and digital terrain models (DTMs) of several regions.
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Correlation of multi-temporal ground-based optical images for landslide monitoring: Application, potential and limitations

TL;DR: In this paper, a low-cost methodology to monitor the displacement of continuously active landslides from ground-based optical images analyzed with a normalized image correlation technique is presented, which can be routinely and automatically applied for operational applications like, for instance, in early warning systems.
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Hydrological response of weathered clay-shale slopes: water infiltration monitoring with time-lapse electrical resistivity tomography

TL;DR: In this paper, an attempt to monitor water infiltration and subsurface flow within a clay-shale landslide using time-lapse electrical resistivity tomography (ERT) is presented.
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Characterization of the 3D geometry of flow-like landslides: A methodology based on the integration of heterogeneous multi-source data

TL;DR: This work presents a methodology for integrating multi-source and multi-resolution data in a 3D geometrical model using geostatistical tools and highlights the influence of the bedrock geometry on the observed kinematic pattern.
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Image-based correlation of Laser Scanning point cloud time series for landslide monitoring

TL;DR: It is demonstrated that pore water pressure changes within the landslide is the main controlling factor of the kinematics and 3D deformation and displacement patterns from repeated TLS surveys.