Articles | Volume 28, issue 20
https://doi.org/10.5194/hess-28-4771-2024
https://doi.org/10.5194/hess-28-4771-2024
Research article
 | 
29 Oct 2024
Research article |  | 29 Oct 2024

Inferring sediment-discharge event types in an Alpine catchment from sub-daily time series

Amalie Skålevåg, Oliver Korup, and Axel Bronstert

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This preprint is open for discussion and under review for Hydrology and Earth System Sciences (HESS).
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Cited articles

Adler, C., Wester, P., Bhatt, I., Huggel, C., Insarov, G., Morecroft, M., Muccione, V., and Prakash, A.: Cross-Chapter Paper 5: Mountains, in: Climate Change 2022: Impacts, Adaptation and Vulnerability, edited by Pörtner, H.-O., Roberts, D., Tignor, M., Poloczanska, E., Mintenbeck, K., Alegría, A., Craig, M., Langsdorf, S., Löschke, S., Möller, V., Okem, A., and Rama, B., 2273–2318, Cambridge University Press, Cambridge, UK and New York, NY, USA, https://doi.org/10.1017/9781009325844.022, 2022. a
Aich, V., Zimmermann, A., and Elsenbeer, H.: Quantification and interpretation of suspended-sediment discharge hysteresis patterns: How much data do we need?, CATENA, 122, 120–129, https://doi.org/10.1016/j.catena.2014.06.020, 2014. a, b
Antoniazza, G. and Lane, S. N.: Sediment yield over glacial cycles: A conceptual model, Prog. Phys. Geog., 45, 842–865, https://doi.org/10.1177/0309133321997292, 2021. a
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. a
Ballantyne, C. K.: Paraglacial geomorphology, Quaternary Sci. Rev., 21, 1935–2017, https://doi.org/10.1016/S0277-3791(02)00005-7, 2002. a
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Short summary
We present a cluster-based approach for inferring sediment discharge event types from suspended sediment concentration and streamflow. Applying it to a glacierised catchment, we find event magnitude and shape complexity to be the key characteristics separating event types, while hysteresis is less important. The four event types are attributed to compound rainfall–melt extremes, high snowmelt and glacier melt, freeze–thaw-modulated snow-melt and precipitation, and late-season glacier melt.
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