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

Viewed

Total article views: 2,800 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,540 1,147 113 2,800 111 102
  • HTML: 1,540
  • PDF: 1,147
  • XML: 113
  • Total: 2,800
  • BibTeX: 111
  • EndNote: 102
Views and downloads (calculated since 18 Jan 2016)
Cumulative views and downloads (calculated since 18 Jan 2016)

Cited

Saved (preprint)

Latest update: 26 Jul 2024
Download
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.
Altmetrics
Final-revised paper
Preprint