Articles | Volume 20, issue 5
https://doi.org/10.5194/nhess-20-1247-2020
https://doi.org/10.5194/nhess-20-1247-2020
Research article
 | 
11 May 2020
Research article |  | 11 May 2020

Erosion after an extreme storm event in an arid fluvial system of the southern Atacama Desert: an assessment of the magnitude, return time, and conditioning factors of erosion and debris flow generation

Germán Aguilar, Albert Cabré, Victor Fredes, and Bruno Villela

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Latest update: 28 Mar 2024
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Short summary
We have calculated erosion caused by an extreme storm in the Atacama Desert. Erosion distribution depends on the ability of catchments to store sediments in stream networks between storms and generate debris flows during the storm. The order of magnitude of erosion is the same as the erosion rates calculated over the long term, so these storms have a relevant influence on the evolution of these arid fluvial systems.
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