When do rock glacier fronts fail? Insights from two case studies in South Tyrol (Italian Alps)

Kofler, Christian, Mair, Volkmar, Gruber, Stephan, Todisco, Maria C., Nettleton, Ian, Steger, Stefan, Zebisch, Marc, Schneiderbauer, Stefan and Comiti, Francesco, (2021). When do rock glacier fronts fail? Insights from two case studies in South Tyrol (Italian Alps). Earth Surface Processes and Landforms, 1-17

Document type:
Article
Collection:
UNU-EHS Articles

Metadata
Documents
Links
Versions
Statistics
  • Attached Files (Some files may be inaccessible until you login with your UNU Collections credentials)
    Name Description MIMEType Size Downloads
    KoflerEtAl_2021_META.pdf KoflerEtAl_2021_META.pdf application/pdf 13.09MB
  • Sub-type Journal article
    Author Kofler, Christian
    Mair, Volkmar
    Gruber, Stephan
    Todisco, Maria C.
    Nettleton, Ian
    Steger, Stefan
    Zebisch, Marc
    Schneiderbauer, Stefan
    Comiti, Francesco
    Title When do rock glacier fronts fail? Insights from two case studies in South Tyrol (Italian Alps)
    Appearing in Earth Surface Processes and Landforms
    Publication Date 2021-02-16
    Place of Publication London
    Publisher John Wiley & Sons Ltd
    Start page 1
    End page 17
    Language eng
    Abstract The fronts of two rock glaciers located in South Tyrol (Italian Alps) failed on 13 August 2014, initiating debris flows in their downslope channels. A multimethod approach including climate, meteorological, and ground temperature data analysis, aerial image correlation, as well as geotechnical testing and modeling, led to the reconstruction of the two events. An integrated investigation of static predisposing factors, slowly changing preparatory factors, and potential triggering events shed light on the most likely reasons for such failures. Our results suggest that the occurrence of front destabilization at the two rock glaciers can only partly be explained by the occurrence of heavy rainfall events. Indeed, antecedent hydrological and thermal ground conditions were characterized by a saturated active layer favored by a snow-rich winter and extensive precipitation in late spring and summer. Also, the rising trend of air temperature during spring and summer months since 1950s might explain the concurrent marked displacement of the two rock glaciers. Indeed, geotechnical investigations have provided strong indications that one of the investigated rock glacier fronts was at a marginally stable state prior to 2014. As rainfall events more intense than the one that occurred in August 2014 were previously recorded in the same area without resulting failures at the studied rock glaciers, we propose that both predisposing and preparatory destabilizing factors have played a key role in the 2014 rock glacier front failures.
    Copyright Holder The Authors
    Copyright Year 2021
    Copyright type Creative commons
  • Versions
    Version Filter Type
  • Citation counts
    Google Scholar Search Google Scholar
    Access Statistics: 594 Abstract Views, 206 File Downloads  -  Detailed Statistics
    Created: Tue, 06 Apr 2021, 19:00:09 JST by Austin Gonzales on behalf of UNU EHS