Articles | Volume 8, issue 3
https://doi.org/10.5194/esurf-8-729-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/esurf-8-729-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Current glacier recession causes significant rockfall increase: the immediate paraglacial response of deglaciating cirque walls
Ingo Hartmeyer
CORRESPONDING AUTHOR
GEORESEARCH Research Institute, Wals, Austria
Robert Delleske
GEORESEARCH Research Institute, Wals, Austria
Markus Keuschnig
GEORESEARCH Research Institute, Wals, Austria
Michael Krautblatter
Chair of Landslide Research, Technical University of Munich, Munich, Germany
Andreas Lang
Department of Geography and Geology, University of Salzburg, Salzburg, Austria
Lothar Schrott
Department of Geography, University of Bonn, Bonn, Germany
Jan-Christoph Otto
Department of Geography and Geology, University of Salzburg, Salzburg, Austria
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43 citations as recorded by crossref.
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- Temporal evolution of headwall erosion rates derived from cosmogenic nuclide concentrations in the medial moraines of Glacier d'Otemma, Switzerland K. Wetterauer et al. 10.1002/esp.5386
- Challenges Facing the Use of Remote Sensing Technologies in the Construction Industry: A Review A. Almohsen 10.3390/buildings14092861
- Climate change related processes affecting mountaineering itineraries, mapping and application to the Valais Alps (Switzerland) J. Mourey et al. 10.1080/04353676.2022.2064651
- Rock temperature variability in high-altitude rockfall-prone areas G. Nigrelli et al. 10.1007/s11629-021-7073-z
- High mountain rockfall dynamics: rockfall activity and runout assessment under the aspect of a changing cryosphere B. Knoflach et al. 10.1080/04353676.2020.1864947
- Assessing the utility of regionalized rock-mass geomechanical properties in rockfall susceptibility modelling in an alpine environment G. Bajni et al. 10.1016/j.geomorph.2022.108401
- High-resolution debris-cover mapping using UAV-derived thermal imagery: limits and opportunities D. Gök et al. 10.5194/tc-17-1165-2023
- Influences Driving and Limiting the Efficacy of Ice Segregation in Alpine Rocks T. Mayer et al. 10.1029/2023GL102951
- Alpine rockwall erosion patterns follow elevation-dependent climate trajectories D. Draebing et al. 10.1038/s43247-022-00348-2
- Ice-buttressing-controlled rock slope failure on a cirque headwall, Lake District, UK P. Carling et al. 10.5194/esurf-11-817-2023
- Assessing the rock failure return period on an unstable Alpine rock wall based on volume-frequency relationships: The Brenva Spur (3916 m a.s.l., Aosta Valley, Italy) L. Fei et al. 10.1016/j.enggeo.2023.107239
- Spatial and temporal variations in rockwall erosion rates derived from cosmogenic 10Be in medial moraines at five valley glaciers around Pigne d'Arolla, Switzerland K. Wetterauer & D. Scherler 10.5194/esurf-11-1013-2023
- Investigation of the 2010 rock avalanche onto the regenerated glacier Brenndalsbreen, Norway S. Engen et al. 10.1007/s10346-024-02275-z
- Volume, evolution, and sedimentation of future glacier lakes in Switzerland over the 21st century T. Steffen et al. 10.5194/esurf-10-723-2022
- 4D quantification of alpine permafrost degradation in steep rock walls using a laboratory‐calibrated electrical resistivity tomography approach R. Scandroglio et al. 10.1002/nsg.12149
- Intensified paraglacial slope failures due to accelerating downwasting of a temperate glacier in Mt. Gongga, southeastern Tibetan Plateau Y. Zhong et al. 10.5194/esurf-10-23-2022
- The evolution of “riskscapes”: 100 years of climate change and mountaineering activity in the Lake Louise area of the Canadian Rockies K. Hanly & G. McDowell 10.1007/s10584-024-03698-2
- Pronounced increase in slope instability linked to global warming: A case study from the eastern European Alps S. Savi et al. 10.1002/esp.5100
- Topographic signatures of progressive glacial landscape transformation M. Liebl et al. 10.1002/esp.5139
- Alpine relief limited by glacial occupation time B. Salcher et al. 10.1130/G48639.1
- Projecting sediment export from two highly glacierized alpine catchments under climate change: exploring non-parametric regression as an analysis tool L. Schmidt et al. 10.5194/hess-28-139-2024
- From Rockfall Observation to Operational Solutions: Nearly 20 years of Cryo-gravitational Hazard Studies in Mont-Blanc Massif F. Magnin et al. 10.4000/rga.11703
- The temperature-dependent shear strength of ice-filled joints in rock mass considering the effect of joint roughness, opening and shear rates S. Huang et al. 10.5194/tc-17-1205-2023
- Vegetation Ecology of Debris-Covered Glaciers (DCGs)—Site Conditions, Vegetation Patterns and Implications for DCGs Serving as Quaternary Cold- and Warm-Stage Plant Refugia T. Fickert et al. 10.3390/d14020114
- High-Temporal-Resolution Rock Slope Monitoring Using Terrestrial Structure-from-Motion Photogrammetry in an Application with Spatial Resolution Limitations B. Butcher et al. 10.3390/rs16010066
- Warming-driven erosion and sediment transport in cold regions T. Zhang et al. 10.1038/s43017-022-00362-0
- Spatiotemporal variations in frost cracking measures in two dimensions: A case study for rock walls in Jotunheimen, southern Norway J. Czekirda et al. 10.1016/j.geomorph.2024.109112
- Spatial and temporal distribution of landslide-dammed lakes in Purlung Tsangpo H. Wang et al. 10.1016/j.enggeo.2022.106802
- Rock and ice avalanche-generated catastrophic debris flow at Chamoli, 7 February 2021: New insights from the geomorphic perspective H. Wang et al. 10.1016/j.geomorph.2024.109110
- Rockfall, glacier recession, and permafrost degradation: long-term monitoring of climate change impacts at the Open-Air-Lab Kitzsteinhorn, Hohe Tauern I. Hartmeyer & J. Otto 10.5194/deuquasp-5-3-2024
- 18-years of high-Alpine rock wall monitoring using terrestrial laser scanning at the Tour Ronde east face, Mont-Blanc massif L. Courtial-Manent et al. 10.1088/1748-9326/ad281d
- Glaciogenic Periglacial Landform in the Making—Geomorphological Evolution of a Rockfall on a Small Glacier in the Horlachtal, Stubai Alps, Austria F. Fleischer et al. 10.3390/rs15061472
- Experimental investigation and strength model of rough ice-filled joints under tensile and shear loading S. Huang et al. 10.1016/j.enggeo.2023.107303
- Holocene warming of alpine rockwalls decreased rockwall erosion rates D. Draebing et al. 10.1016/j.epsl.2023.118496
- Evaluation of rockfall trends at a sedimentary rock cut near Manitou Springs, Colorado, using daily photogrammetric monitoring G. Walton et al. 10.1007/s10346-023-02121-8
- De l’observation des écroulements aux solutions opérationnelles : près de deux décennies d’études sur les risques cryo-gravitaires dans le massif du Mont-Blanc F. Magnin et al. 10.4000/rga.11644
- Ice aprons on steep high-alpine slopes: insights from the Mont-Blanc massif, Western Alps L. Ravanel et al. 10.1017/jog.2023.15
- The concept of event-size-dependent exhaustion and its application to paraglacial rockslides S. Hergarten 10.5194/nhess-23-3051-2023
- Sedimentary organic molecular compositions reveal the influence of glacier retreat on ecology on the Tibetan Plateau S. Shi et al. 10.1016/j.scitotenv.2023.163629
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- Multi-method monitoring of rockfall activity along the classic route up Mont Blanc (4809 m a.s.l.) to encourage adaptation by mountaineers J. Mourey et al. 10.5194/nhess-22-445-2022
2 citations as recorded by crossref.
- Deciphering meteorological influencing factors for Alpine rockfalls: a case study in Aosta Valley G. Bajni et al. 10.1007/s10346-021-01697-3
- Rockfall hazard estimation and related applications for a preliminary risk assessment at regional scale: an example from northwestern Italian Alps D. Tiranti et al. 10.1007/s10346-023-02060-4
Latest update: 14 Nov 2024
Short summary
Climate warming is causing significant ice surface lowering even in the uppermost parts of alpine glaciers. Using terrestrial lidar, we quantify rockfall in freshly exposed cirque walls. During 6-year monitoring (2011–2017), an extensive dataset was established and over 600 rockfall events identified. Drastically increased rockfall activity following ice retreat can clearly be observed as 60 % of the rockfall volume detached from less than 10 m above the glacier surface.
Climate warming is causing significant ice surface lowering even in the uppermost parts of...