Articles | Volume 11, issue 3
https://doi.org/10.5194/esurf-11-383-2023
https://doi.org/10.5194/esurf-11-383-2023
Research article
 | 
08 May 2023
Research article |  | 08 May 2023

Evolution of an Alpine proglacial river during 7 decades of deglaciation

Livia Piermattei, Tobias Heckmann, Sarah Betz-Nutz, Moritz Altmann, Jakob Rom, Fabian Fleischer, Manuel Stark, Florian Haas, Camillo Ressl, Michael H. Wimmer, Norbert Pfeifer, and Michael Becht

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Cited articles

Altmann, M., Piermattei, L., Haas, F., Heckmann, T., Fleischer, F., Rom, J., Betz-Nutz, S., Knoflach, B., Müller, S., Ramskogler, K., Pfeiffer, M., Hofmeister, F., Ressl, C., and Becht, M.: Long-Term Changes of Morphodynamics on Little Ice Age Lateral Moraines and the Resulting Sediment Transfer into Mountain Streams in the Upper Kauner Valley, Austria, Water, 12, 3375, https://doi.org/10.3390/w12123375, 2020. 
Anderson, S. W.: Uncertainty in quantitative analyses of topographic change: error propagation and the role of thresholding, Earth Surf. Proc. Land., 44, 1015–1033, https://doi.org/10.1002/esp.4551, 2019. 
Anderson, S. W. and Shean, D.: Spatial and temporal controls on proglacial erosion rates: A comparison of four basins on Mount Rainier, 1960 to 2017, Earth Surf. Proc. Land., 47, 596–617, https://doi.org/10.1002/esp.5274, 2022. 
Antoniazza, G., Nicollier, T., Boss, S., Mettra, F., Badoux, A., Schaefli, B., Rickenmann, D., and Lane, S. N.: Hydrological Drivers of Bedload Transport in an Alpine Watershed, Water Resour. Res., 58, e2021WR030663, https://doi.org/10.1029/2021WR030663, 2022. 
Ashworth, P. J. and Ferguson, R. I.: Interrelationships of Channel Processes, Changes and Sediments in a Proglacial Braided River, Geogr. Ann. A, 68, 361–371, https://doi.org/10.1080/04353676.1986.11880186, 1986. 
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Short summary
Alpine rivers have experienced strong changes over the last century. In the present study, we explore the potential of historical multi-temporal elevation models, combined with recent topographic data, to quantify 66 years (from 1953 to 2019) of river changes in the glacier forefield of an Alpine catchment. Thereby, we quantify the changes in the river form as well as the related sediment erosion and deposition.
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