Impacts of climate and reservoirs on the downstream design flood hydrograph: a case study of Yichang Station

The Upper Yangtze River (above Yichang) in China has constructed the world's largest reservoir group with the Three Gorges Reservoir (TGR) as the core, the operation of these reservoirs and future climate change will no doubt alter the downstream hydrological processes and pose a challenge to t...

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Veröffentlicht in:Natural hazards (Dordrecht) 2022-09, Vol.113 (3), p.1803-1831
Hauptverfasser: Li, Rongrong, Xiong, Lihua, Zha, Xini, Xiong, Bin, Liu, Han, Chen, Jie, Zeng, Ling, Li, Wenbin
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Xiong, Lihua
Zha, Xini
Xiong, Bin
Liu, Han
Chen, Jie
Zeng, Ling
Li, Wenbin
description The Upper Yangtze River (above Yichang) in China has constructed the world's largest reservoir group with the Three Gorges Reservoir (TGR) as the core, the operation of these reservoirs and future climate change will no doubt alter the downstream hydrological processes and pose a challenge to the downstream flood design. As Yichang Hydrologic Station is 44 km downstream of TGR, how the design flood at Yichang Station would be impacted in the future by climate and upstream reservoirs has rarely been investigated. In this study, the climate and upstream reservoirs effects on design flood at Yichang Station are evaluated under six future climate and reservoir scenarios (S1, S2, S3, S4, S5 and S6) with different combinations of summer precipitation anomaly (SPA) and reservoir index (RI), in which SPA is obtained from global climate models under the three emission scenarios (SSP1-2.6, SSP2-4.5 and SSP5-8.5) of CMIP6 and RI is calculated under the two reservoir conditions (RI at current level and RI at planning level). The SPA and RI of S1, S2, S3, S4, S5 and S6 are, respectively, substituted into the optimal nonstationary GEV probability model, and the corresponding 1000-year design floods are estimated by using average annual reliability method. Under the same future reservoir condition, the flood peak discharge, 3-day, 7-day, 15-day and 30-day flood volume (denoted as Q m , W 3 , W 7 , W 15 and W 30 , respectively) under SSP2-4.5 and SSP5-8.5 are 0.2% ~ 2.5% larger than those under SSP1-2.6. The change rates of Q m , W 3 , W 7 , W 15 and W 30 under six scenarios relative to the stationary design flood values calculated by Changjiang Water Resources Commission range from −11.4% to −23.9%, and the reduction amount of Q m is more than 16,000 m 3 /s even under SSP5-8.5. Therefore, reservoirs impact on the design flood of Yichang Station is quite prominent.
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As Yichang Hydrologic Station is 44 km downstream of TGR, how the design flood at Yichang Station would be impacted in the future by climate and upstream reservoirs has rarely been investigated. In this study, the climate and upstream reservoirs effects on design flood at Yichang Station are evaluated under six future climate and reservoir scenarios (S1, S2, S3, S4, S5 and S6) with different combinations of summer precipitation anomaly (SPA) and reservoir index (RI), in which SPA is obtained from global climate models under the three emission scenarios (SSP1-2.6, SSP2-4.5 and SSP5-8.5) of CMIP6 and RI is calculated under the two reservoir conditions (RI at current level and RI at planning level). The SPA and RI of S1, S2, S3, S4, S5 and S6 are, respectively, substituted into the optimal nonstationary GEV probability model, and the corresponding 1000-year design floods are estimated by using average annual reliability method. Under the same future reservoir condition, the flood peak discharge, 3-day, 7-day, 15-day and 30-day flood volume (denoted as Q m , W 3 , W 7 , W 15 and W 30 , respectively) under SSP2-4.5 and SSP5-8.5 are 0.2% ~ 2.5% larger than those under SSP1-2.6. The change rates of Q m , W 3 , W 7 , W 15 and W 30 under six scenarios relative to the stationary design flood values calculated by Changjiang Water Resources Commission range from −11.4% to −23.9%, and the reduction amount of Q m is more than 16,000 m 3 /s even under SSP5-8.5. 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Under the same future reservoir condition, the flood peak discharge, 3-day, 7-day, 15-day and 30-day flood volume (denoted as Q m , W 3 , W 7 , W 15 and W 30 , respectively) under SSP2-4.5 and SSP5-8.5 are 0.2% ~ 2.5% larger than those under SSP1-2.6. The change rates of Q m , W 3 , W 7 , W 15 and W 30 under six scenarios relative to the stationary design flood values calculated by Changjiang Water Resources Commission range from −11.4% to −23.9%, and the reduction amount of Q m is more than 16,000 m 3 /s even under SSP5-8.5. 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As Yichang Hydrologic Station is 44 km downstream of TGR, how the design flood at Yichang Station would be impacted in the future by climate and upstream reservoirs has rarely been investigated. In this study, the climate and upstream reservoirs effects on design flood at Yichang Station are evaluated under six future climate and reservoir scenarios (S1, S2, S3, S4, S5 and S6) with different combinations of summer precipitation anomaly (SPA) and reservoir index (RI), in which SPA is obtained from global climate models under the three emission scenarios (SSP1-2.6, SSP2-4.5 and SSP5-8.5) of CMIP6 and RI is calculated under the two reservoir conditions (RI at current level and RI at planning level). The SPA and RI of S1, S2, S3, S4, S5 and S6 are, respectively, substituted into the optimal nonstationary GEV probability model, and the corresponding 1000-year design floods are estimated by using average annual reliability method. Under the same future reservoir condition, the flood peak discharge, 3-day, 7-day, 15-day and 30-day flood volume (denoted as Q m , W 3 , W 7 , W 15 and W 30 , respectively) under SSP2-4.5 and SSP5-8.5 are 0.2% ~ 2.5% larger than those under SSP1-2.6. The change rates of Q m , W 3 , W 7 , W 15 and W 30 under six scenarios relative to the stationary design flood values calculated by Changjiang Water Resources Commission range from −11.4% to −23.9%, and the reduction amount of Q m is more than 16,000 m 3 /s even under SSP5-8.5. Therefore, reservoirs impact on the design flood of Yichang Station is quite prominent.</abstract><cop>Dordrecht</cop><pub>Springer Netherlands</pub><doi>10.1007/s11069-022-05370-3</doi><tpages>29</tpages><orcidid>https://orcid.org/0000-0001-6990-2414</orcidid></addata></record>
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subjects Canyons
Civil Engineering
Climate change
Climate models
Design
Design floods
Downstream
Earth and Environmental Science
Earth Sciences
Environmental Management
Flood hydrographs
Flood peak
Floods
Future climates
Geophysics/Geodesy
Geotechnical Engineering & Applied Earth Sciences
Global climate
Global climate models
Hydrogeology
Hydrographs
Hydrologic processes
Hydrology
Natural Hazards
Original Paper
Precipitation anomalies
Probability theory
Reliability aspects
Reservoirs
Summer precipitation
Upstream
Water resources
title Impacts of climate and reservoirs on the downstream design flood hydrograph: a case study of Yichang Station
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