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Lorenzo Picco

Researcher at Austral University of Chile

Publications -  83
Citations -  1266

Lorenzo Picco is an academic researcher from Austral University of Chile. The author has contributed to research in topics: Fluvial & Sediment. The author has an hindex of 16, co-authored 83 publications receiving 923 citations. Previous affiliations of Lorenzo Picco include University of Padua.

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Channel adjustments and vegetation cover dynamics in a large gravel bed river over the last 200 years

TL;DR: In this article, the authors analyzed the evolution of the Piave River in the last 200 years using historical maps, aerial photos, repeated topographic measurements, and geomorphological surveys.
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Tracking log displacement during floods in the Tagliamento River using RFID and GPS tracker devices

TL;DR: In this paper, the authors used GPS tracker devices to monitor the entrainment and movements of logs in large gravel-bed rivers during floods, revealing the potentials of GPS trackers for better planning of river management practices and strategies involving the use of large wood pieces and could help for calibrating wood budgets at reach scale.
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Three decades of monitoring in the Rio Cordon instrumented basin: Sediment budget and temporal trend of sediment yield

TL;DR: In this article, the authors investigated sediment fluxes in an instrumented Alpine basin (Rio Cordon, Italy) and analyzed sediment dynamics at different time scales, ranging from short (single event) to long-term (three decades).
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Evaluating short-term morphological changes in a gravel-bed braided river using terrestrial laser scanner

TL;DR: In this paper, the authors analyzed the short-term morphological dynamics and the processes of erosion and sediment deposition along a small reach of a relatively unimpacted gravel-bed braided river (Tagliamento River, northeast Italy) using a terrestrial laser scanner.
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Channel adjustments and island dynamics in the brenta river (italy) over the last 30 years

TL;DR: In this paper, the authors analyzed the timing and extent of plan-form morphological changes that occurred over the last 30 years along the middle portion of the Brenta River (20km long) through the examination of aerial photos, repeated topographic measurements and hydrological data.