Towards a sediment transfer capacity index of rock glaciers: Examples from two catchments in South Tyrol, (Eastern Italian Alps)

Kofler, Christian, Mair, Volkmar, Comiti, Francesco, Zebisch, Marc, Schneiderbauer, Stefan and Steger, Stefan, (2022). Towards a sediment transfer capacity index of rock glaciers: Examples from two catchments in South Tyrol, (Eastern Italian Alps). Catena, 216 1-14

Document type:
Article
Collection:

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
    n1-s2.0-S0341816222003150-main.pdf 1-s2.0-S0341816222003150-main.pdf Click to show the corresponding preview/stream application/pdf; 15.86MB
  • Sub-type Journal article
    Author Kofler, Christian
    Mair, Volkmar
    Comiti, Francesco
    Zebisch, Marc
    Schneiderbauer, Stefan
    Steger, Stefan
    Title Towards a sediment transfer capacity index of rock glaciers: Examples from two catchments in South Tyrol, (Eastern Italian Alps)
    Appearing in Catena
    Volume 216
    Publication Date 2022-09
    Place of Publication Amsterdam
    Publisher Elsevier
    Start page 1
    End page 14
    Language eng
    Abstract Rock glaciers are active sediment transport systems of high mountain periglacial environments. Driven by the internal deformation of their frozen core, they can convey substantial amounts of debris from their nourishing zone towards their front. Depending on the topographic conditions at the front slope, the released sediment is either overridden again by the advancing rock glacier or transferred downwards by rapid mass movements. The capacity of rock glacier environments to transfer sediment however has remained largely unexplored, in particular beyond the local scale. In this work, we consider a rock glaciers’ sediment transfer capacity as a function of its transported volume rate and the travel range of mobilized material at its front. A GIS-based method, low in data-demand, is proposed to generate catchment-scale proxies for the above-mentioned input variables and to combine them to a qualitative index describing sediment transfer capacity of rock glacier fronts. The proposed method is applied in two basins, strongly characterized by periglacial dynamics (Ultental and Schnalstal in South Tyrol, Eastern Italian Alps). In a final step, computed sediment transfer classes are assessed on their geomorphological plausibility by building empirical relationships with independent environmental variables.
    Keyword Sediment transport
    Permafrost
    Debris flows
    Periglacial geomorphology
    Copyright Holder The Authors
    Copyright Year 2022
    Copyright type Creative commons
    DOI 10.1016/j.catena.2022.106329
  • Versions
    Version Filter Type
  • Citation counts
    Google Scholar Search Google Scholar
    Access Statistics: 210 Abstract Views, 66 File Downloads  -  Detailed Statistics
    Created: Wed, 04 Jan 2023, 22:31:55 JST by Aarti Basnyat on behalf of UNU EHS