The role of thermokarst evolution in debris flow initiation (Hüttekar Rock Glacier, Austrian Alps)
A rapid sequence of cascading events involving thermokarst lake outburst, local rock glacier front failure, debris flow development, and river blockage hit Radurschl Valley (Ötztal Alps, Tyrol) on 13 August 2019. Compounding effects from permafrost degradation and drainage network development within...
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ftcopernicus:oai:publications.copernicus.org:nhess104883 2023-08-15T12:42:47+02:00 The role of thermokarst evolution in debris flow initiation (Hüttekar Rock Glacier, Austrian Alps) Seelig, Simon Wagner, Thomas Krainer, Karl Avian, Michael Olefs, Marc Haslinger, Klaus Winkler, Gerfried 2023-07-20 application/pdf https://doi.org/10.5194/nhess-23-2547-2023 https://nhess.copernicus.org/articles/23/2547/2023/ eng eng doi:10.5194/nhess-23-2547-2023 https://nhess.copernicus.org/articles/23/2547/2023/ eISSN: 1684-9981 Text 2023 ftcopernicus https://doi.org/10.5194/nhess-23-2547-2023 2023-07-24T16:24:16Z A rapid sequence of cascading events involving thermokarst lake outburst, local rock glacier front failure, debris flow development, and river blockage hit Radurschl Valley (Ötztal Alps, Tyrol) on 13 August 2019. Compounding effects from permafrost degradation and drainage network development within the rock glacier initiated the complex process chain. The debris flow dammed the main river of the valley, impounding a water volume of 120 000 m 3 that was partly drained by excavation to prevent a potentially catastrophic outburst flood. We present a systematic analysis of destabilizing factors to deduce the failure mechanism. The identification and evaluation of individual factors reveals a critical combination of topographical and sedimentological disposition, climate, and weather patterns driving the evolution of a thermokarst drainage network. Progressively changing groundwater flow and storage patterns within the frozen sediment accumulation governed the slope stability of the rock glacier front. Our results demonstrate the hazard potential of active rock glaciers due to their large amount of mobilizable sediment, dynamically changing internal structure, thermokarst lake development, and substantial water flow along a rapidly evolving channel network. Text permafrost Thermokarst Copernicus Publications: E-Journals Natural Hazards and Earth System Sciences 23 7 2547 2568 |
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Copernicus Publications: E-Journals |
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English |
description |
A rapid sequence of cascading events involving thermokarst lake outburst, local rock glacier front failure, debris flow development, and river blockage hit Radurschl Valley (Ötztal Alps, Tyrol) on 13 August 2019. Compounding effects from permafrost degradation and drainage network development within the rock glacier initiated the complex process chain. The debris flow dammed the main river of the valley, impounding a water volume of 120 000 m 3 that was partly drained by excavation to prevent a potentially catastrophic outburst flood. We present a systematic analysis of destabilizing factors to deduce the failure mechanism. The identification and evaluation of individual factors reveals a critical combination of topographical and sedimentological disposition, climate, and weather patterns driving the evolution of a thermokarst drainage network. Progressively changing groundwater flow and storage patterns within the frozen sediment accumulation governed the slope stability of the rock glacier front. Our results demonstrate the hazard potential of active rock glaciers due to their large amount of mobilizable sediment, dynamically changing internal structure, thermokarst lake development, and substantial water flow along a rapidly evolving channel network. |
format |
Text |
author |
Seelig, Simon Wagner, Thomas Krainer, Karl Avian, Michael Olefs, Marc Haslinger, Klaus Winkler, Gerfried |
spellingShingle |
Seelig, Simon Wagner, Thomas Krainer, Karl Avian, Michael Olefs, Marc Haslinger, Klaus Winkler, Gerfried The role of thermokarst evolution in debris flow initiation (Hüttekar Rock Glacier, Austrian Alps) |
author_facet |
Seelig, Simon Wagner, Thomas Krainer, Karl Avian, Michael Olefs, Marc Haslinger, Klaus Winkler, Gerfried |
author_sort |
Seelig, Simon |
title |
The role of thermokarst evolution in debris flow initiation (Hüttekar Rock Glacier, Austrian Alps) |
title_short |
The role of thermokarst evolution in debris flow initiation (Hüttekar Rock Glacier, Austrian Alps) |
title_full |
The role of thermokarst evolution in debris flow initiation (Hüttekar Rock Glacier, Austrian Alps) |
title_fullStr |
The role of thermokarst evolution in debris flow initiation (Hüttekar Rock Glacier, Austrian Alps) |
title_full_unstemmed |
The role of thermokarst evolution in debris flow initiation (Hüttekar Rock Glacier, Austrian Alps) |
title_sort |
role of thermokarst evolution in debris flow initiation (hüttekar rock glacier, austrian alps) |
publishDate |
2023 |
url |
https://doi.org/10.5194/nhess-23-2547-2023 https://nhess.copernicus.org/articles/23/2547/2023/ |
genre |
permafrost Thermokarst |
genre_facet |
permafrost Thermokarst |
op_source |
eISSN: 1684-9981 |
op_relation |
doi:10.5194/nhess-23-2547-2023 https://nhess.copernicus.org/articles/23/2547/2023/ |
op_doi |
https://doi.org/10.5194/nhess-23-2547-2023 |
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Natural Hazards and Earth System Sciences |
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23 |
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7 |
container_start_page |
2547 |
op_container_end_page |
2568 |
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1774297420137496576 |