Multidecadal Sediment Balance Modelling of a Cascade of Alpine Reservoirs and Perspectives Based on Climate Warming
Abstract
:1. Introduction
- Characterize the present sediment balance of a complex hydropower cascade, by quantifying and modelling the annual sediment inputs and outputs and determining the sedimentation rate of each reservoir.
- Estimate the effects of climate warming on the sediment dynamics of the catchments and assess the future evolution of sediment trapping in the reservoirs by means of the previously established model.
2. Case Study
3. Methodology
3.1. Sediment Yield
- Period I, from 1990 to 2012, for which the parameters are characterized by field measurements.
- Period II, from 2013 to 2065, and Period III, from 2066 to 2099, for which the parameters are characterized by the predictions based on the A1B climate change scenario [22].
3.2. Sedimentation Rate
3.3. Sedimentation Rate for Fine Sediments
3.4. Sedimentation Exchange through Power Waterways
4. Results
4.1. Sediment Yield
4.2. Sedimentation Rate
4.3. Sedimentation Rate of Fine Sediments
4.4. Sediment Fluxes through the Power Waterways
4.5. Sediment Balance at Present
5. Discussion
5.1. Present Situation
5.2. Perspectives Based on Climate Warming
6. Conclusions
Author Contributions
Funding
Acknowledgments
Conflicts of Interest
References
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Characteristics of the Catchments | Oberaar | Grimsel | Räterichsboden | Trift (*) |
---|---|---|---|---|
Surface (km2) | 19.24 | 77.56 | 11.51 | 33.52 |
Max altitude (m a.s.l.) | 3622 | 4262 | 3237 | 3486 |
Mean altitude (m a.s.l.) | 2729 | 2669 | 2426 | 2667 |
Min altitude (m a.s.l.) | 2209 | 1800 | 1650 | 1652 |
Glaciated area in 2012 (%) | 29 | 35 | 0 | 46 |
Maximum supply level (m a.s.l.) | 2303 | 1909 | 1767 | 1767 |
Maximum capacity (hm3) | 62 | 97 | 25 | 85 |
Lake surface (km2) | 1.60 | 2.82 | 0.65 | 1.10 |
Catchment | Period I | Period II | Period III | |||
---|---|---|---|---|---|---|
VA | SY | VA | SY | VA | SY | |
(m³·km−2·year−1) | (m³/year) | (m³·km−2·year−1) | (m³/year) | (m³·km−2·year−1) | (m³/year) | |
Oberaar | 1262 | 24,276 | 1427 | 27,457 | 1407 | 27,064 |
Grimsel | 1068 | 82,869 | 1105 | 85,704 | 1261 | 97,839 |
Räterichsboden | 2204 | 25,365 | 2178 | 25,073 | 2180 | 25,096 |
Trift | 1526 | 51,149 | 1555 | 52,130 | 1745 | 58,504 |
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Guillén-Ludeña, S.; Manso, P.A.; Schleiss, A.J. Multidecadal Sediment Balance Modelling of a Cascade of Alpine Reservoirs and Perspectives Based on Climate Warming. Water 2018, 10, 1759. https://doi.org/10.3390/w10121759
Guillén-Ludeña S, Manso PA, Schleiss AJ. Multidecadal Sediment Balance Modelling of a Cascade of Alpine Reservoirs and Perspectives Based on Climate Warming. Water. 2018; 10(12):1759. https://doi.org/10.3390/w10121759
Chicago/Turabian StyleGuillén-Ludeña, Sebastián, Pedro A. Manso, and Anton J. Schleiss. 2018. "Multidecadal Sediment Balance Modelling of a Cascade of Alpine Reservoirs and Perspectives Based on Climate Warming" Water 10, no. 12: 1759. https://doi.org/10.3390/w10121759