Disentangling human impact from natural controls of sediment dynamics in an Alpine catchment
Disentangling human impact from natural controls of sediment dynamics in an Alpine catchment
Human activities have increasingly strong impacts on the sediment dynamics of watersheds, directly, for example through water abstraction and sediment extraction, but also indirectly through climate change. This study aims at disentangling these impacts on natural sediment fluxes for the Borgne River, located in the Alps of southwest Switzerland, using two approaches: First, an assessment of contemporary sediment sources and their relative contribution to the sediment delivered to the catchment outlet is undertaken by geochemical fingerprinting and a mixing model. Second, a spatially distributed conceptual model of suspended sediment production and transfer is used to quantify the contribution of different portions of the catchment to the total sediment yield. The model describes the influence of hydroclimatic variables (rainfall, snowmelt, and ice melt), water diversions and reservoir trapping on the sediment yield accounting for the erodibility of the different land covers present in the catchment. The analysis of different scenarios based on this conceptual model aids the interpretation of the fingerprinting results and the identification of the most important factors controlling sediment fluxes. Although the conceptual model overestimates the contribution of the downstream source area and underestimates the contribution of the upstream source area, the results allow us to qualitatively assess the impacts of different drivers influencing the sediment yield at the catchment scale. The results suggest: (1) high sediment yield from the uppermost part of the catchment due to sediment delivery by glacial ice melt; (2) delayed sediment transfer from areas impacted by water abstraction; and (3) reduced sediment contribution from areas upstream of a major hydropower reservoir that intercepts and traps sediment. Although process (1) and processes (2) and (3) serve to counter one another, our study emphasizes that the relative impacts of Anthropocene climate change and human impacts on sediment delivery may be disentangled through multi‐proxy approaches.
Stutenbecker, Laura
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Costa, Anna
814cc328-f061-48b8-9df8-17b93d09fa20
Bakker, Maarten
18823566-2d22-4e58-9b51-fb51551a77b1
Anghileri, Daniela
611ecf6c-55d5-4e63-b051-53e2324a7698
Molnar, Peter
99f2d15c-5348-4c80-bb35-fb54c133862d
Lane, Stuart N.
b152c3b1-2381-495d-82e0-c4b199efd148
Schlunegger, Fritz
19b537df-8eb8-45bb-9c5d-ace0491fb019
13 August 2019
Stutenbecker, Laura
93cd9153-c6be-47df-aaf4-db1b729a92af
Costa, Anna
814cc328-f061-48b8-9df8-17b93d09fa20
Bakker, Maarten
18823566-2d22-4e58-9b51-fb51551a77b1
Anghileri, Daniela
611ecf6c-55d5-4e63-b051-53e2324a7698
Molnar, Peter
99f2d15c-5348-4c80-bb35-fb54c133862d
Lane, Stuart N.
b152c3b1-2381-495d-82e0-c4b199efd148
Schlunegger, Fritz
19b537df-8eb8-45bb-9c5d-ace0491fb019
Stutenbecker, Laura, Costa, Anna, Bakker, Maarten, Anghileri, Daniela, Molnar, Peter, Lane, Stuart N. and Schlunegger, Fritz
(2019)
Disentangling human impact from natural controls of sediment dynamics in an Alpine catchment.
Earth Surface Processes and Landforms.
(doi:10.1002/esp.4716).
Abstract
Human activities have increasingly strong impacts on the sediment dynamics of watersheds, directly, for example through water abstraction and sediment extraction, but also indirectly through climate change. This study aims at disentangling these impacts on natural sediment fluxes for the Borgne River, located in the Alps of southwest Switzerland, using two approaches: First, an assessment of contemporary sediment sources and their relative contribution to the sediment delivered to the catchment outlet is undertaken by geochemical fingerprinting and a mixing model. Second, a spatially distributed conceptual model of suspended sediment production and transfer is used to quantify the contribution of different portions of the catchment to the total sediment yield. The model describes the influence of hydroclimatic variables (rainfall, snowmelt, and ice melt), water diversions and reservoir trapping on the sediment yield accounting for the erodibility of the different land covers present in the catchment. The analysis of different scenarios based on this conceptual model aids the interpretation of the fingerprinting results and the identification of the most important factors controlling sediment fluxes. Although the conceptual model overestimates the contribution of the downstream source area and underestimates the contribution of the upstream source area, the results allow us to qualitatively assess the impacts of different drivers influencing the sediment yield at the catchment scale. The results suggest: (1) high sediment yield from the uppermost part of the catchment due to sediment delivery by glacial ice melt; (2) delayed sediment transfer from areas impacted by water abstraction; and (3) reduced sediment contribution from areas upstream of a major hydropower reservoir that intercepts and traps sediment. Although process (1) and processes (2) and (3) serve to counter one another, our study emphasizes that the relative impacts of Anthropocene climate change and human impacts on sediment delivery may be disentangled through multi‐proxy approaches.
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Stutenberg_2019_accepted_version
- Accepted Manuscript
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Accepted/In Press date: 7 August 2019
Published date: 13 August 2019
Identifiers
Local EPrints ID: 434805
URI: http://eprints.soton.ac.uk/id/eprint/434805
ISSN: 0197-9337
PURE UUID: 0b3db012-c270-4edb-98bc-4a77a50364b1
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Date deposited: 09 Oct 2019 16:30
Last modified: 16 Mar 2024 08:13
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Contributors
Author:
Laura Stutenbecker
Author:
Anna Costa
Author:
Maarten Bakker
Author:
Peter Molnar
Author:
Stuart N. Lane
Author:
Fritz Schlunegger
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