Articles | Volume 17, issue 9
https://doi.org/10.5194/nhess-17-1595-2017
https://doi.org/10.5194/nhess-17-1595-2017
Research article
 | 
22 Sep 2017
Research article |  | 22 Sep 2017

A modified tank model including snowmelt and infiltration time lags for deep-seated landslides in alpine environments (Aggenalm, Germany)

Wen Nie, Michael Krautblatter, Kerry Leith, Kurosch Thuro, and Judith Festl

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Short summary
Deep-seated landslides are an important and widespread natural hazard within alpine regions and can have a massive impact on infrastructure. Pore water pressure plays an important role in determining the stability of hydro-triggered deep-seated landslides. Here we demonstrate a modified tank model for deep-seated landslides that includes snow and infiltration effects and can effectively predict changes in pore water pressure in alpine environments.
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