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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creator | Li, Rongrong 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. |
doi_str_mv | 10.1007/s11069-022-05370-3 |
format | Article |
fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_2715333524</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2715333524</sourcerecordid><originalsourceid>FETCH-LOGICAL-c319t-8e29339eccce00c17d278b370acb2717a03f961004c44fe3558cc3ccb86b48a53</originalsourceid><addsrcrecordid>eNp9kE1LAzEQhoMoWKt_wFPA8-ok2U9vUvwoFDyooKeQnc1-lDZZk1Tpvze6gjdPc5j3eYd5CDlncMkAiivPGORVApwnkIkCEnFAZiwrRAJlCodkBhVnCQh4PSYn3q8BGMt5NSOb5XZUGDy1LcXNsFVBU2Ua6rTX7sMOLm4MDb2mjf00PjittrTRfugMbTfWNrTfN852To39NVUUldfUh12z_258G7BXpqNPQYXBmlNy1KqN12e_c05e7m6fFw_J6vF-ubhZJShYFZJS80qISiOiBkBWNLwo6_iVwpoXrFAg2iqPf6eYpq0WWVYiCsS6zOu0VJmYk4upd3T2fad9kGu7cyaelJHPhBAZT2OKTyl01nunWzm6KMDtJQP5bVVOVmW0Kn-sShEhMUE-hk2n3V_1P9QXQMV7GA</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2715333524</pqid></control><display><type>article</type><title>Impacts of climate and reservoirs on the downstream design flood hydrograph: a case study of Yichang Station</title><source>SpringerLink (Online service)</source><creator>Li, Rongrong ; Xiong, Lihua ; Zha, Xini ; Xiong, Bin ; Liu, Han ; Chen, Jie ; Zeng, Ling ; Li, Wenbin</creator><creatorcontrib>Li, Rongrong ; Xiong, Lihua ; Zha, Xini ; Xiong, Bin ; Liu, Han ; Chen, Jie ; Zeng, Ling ; Li, Wenbin</creatorcontrib><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.</description><identifier>ISSN: 0921-030X</identifier><identifier>EISSN: 1573-0840</identifier><identifier>DOI: 10.1007/s11069-022-05370-3</identifier><language>eng</language><publisher>Dordrecht: Springer Netherlands</publisher><subject>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</subject><ispartof>Natural hazards (Dordrecht), 2022-09, Vol.113 (3), p.1803-1831</ispartof><rights>The Author(s), under exclusive licence to Springer Nature B.V. 2022</rights><rights>The Author(s), under exclusive licence to Springer Nature B.V. 2022.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c319t-8e29339eccce00c17d278b370acb2717a03f961004c44fe3558cc3ccb86b48a53</citedby><cites>FETCH-LOGICAL-c319t-8e29339eccce00c17d278b370acb2717a03f961004c44fe3558cc3ccb86b48a53</cites><orcidid>0000-0001-6990-2414</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s11069-022-05370-3$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s11069-022-05370-3$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Li, Rongrong</creatorcontrib><creatorcontrib>Xiong, Lihua</creatorcontrib><creatorcontrib>Zha, Xini</creatorcontrib><creatorcontrib>Xiong, Bin</creatorcontrib><creatorcontrib>Liu, Han</creatorcontrib><creatorcontrib>Chen, Jie</creatorcontrib><creatorcontrib>Zeng, Ling</creatorcontrib><creatorcontrib>Li, Wenbin</creatorcontrib><title>Impacts of climate and reservoirs on the downstream design flood hydrograph: a case study of Yichang Station</title><title>Natural hazards (Dordrecht)</title><addtitle>Nat Hazards</addtitle><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.</description><subject>Canyons</subject><subject>Civil Engineering</subject><subject>Climate change</subject><subject>Climate models</subject><subject>Design</subject><subject>Design floods</subject><subject>Downstream</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Environmental Management</subject><subject>Flood hydrographs</subject><subject>Flood peak</subject><subject>Floods</subject><subject>Future climates</subject><subject>Geophysics/Geodesy</subject><subject>Geotechnical Engineering & Applied Earth Sciences</subject><subject>Global climate</subject><subject>Global climate models</subject><subject>Hydrogeology</subject><subject>Hydrographs</subject><subject>Hydrologic processes</subject><subject>Hydrology</subject><subject>Natural Hazards</subject><subject>Original Paper</subject><subject>Precipitation anomalies</subject><subject>Probability theory</subject><subject>Reliability aspects</subject><subject>Reservoirs</subject><subject>Summer precipitation</subject><subject>Upstream</subject><subject>Water resources</subject><issn>0921-030X</issn><issn>1573-0840</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp9kE1LAzEQhoMoWKt_wFPA8-ok2U9vUvwoFDyooKeQnc1-lDZZk1Tpvze6gjdPc5j3eYd5CDlncMkAiivPGORVApwnkIkCEnFAZiwrRAJlCodkBhVnCQh4PSYn3q8BGMt5NSOb5XZUGDy1LcXNsFVBU2Ua6rTX7sMOLm4MDb2mjf00PjittrTRfugMbTfWNrTfN852To39NVUUldfUh12z_258G7BXpqNPQYXBmlNy1KqN12e_c05e7m6fFw_J6vF-ubhZJShYFZJS80qISiOiBkBWNLwo6_iVwpoXrFAg2iqPf6eYpq0WWVYiCsS6zOu0VJmYk4upd3T2fad9kGu7cyaelJHPhBAZT2OKTyl01nunWzm6KMDtJQP5bVVOVmW0Kn-sShEhMUE-hk2n3V_1P9QXQMV7GA</recordid><startdate>20220901</startdate><enddate>20220901</enddate><creator>Li, Rongrong</creator><creator>Xiong, Lihua</creator><creator>Zha, Xini</creator><creator>Xiong, Bin</creator><creator>Liu, Han</creator><creator>Chen, Jie</creator><creator>Zeng, Ling</creator><creator>Li, Wenbin</creator><general>Springer Netherlands</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7ST</scope><scope>7TG</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>M2P</scope><scope>M7S</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>SOI</scope><orcidid>https://orcid.org/0000-0001-6990-2414</orcidid></search><sort><creationdate>20220901</creationdate><title>Impacts of climate and reservoirs on the downstream design flood hydrograph: a case study of Yichang Station</title><author>Li, Rongrong ; Xiong, Lihua ; Zha, Xini ; Xiong, Bin ; Liu, Han ; Chen, Jie ; Zeng, Ling ; Li, Wenbin</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c319t-8e29339eccce00c17d278b370acb2717a03f961004c44fe3558cc3ccb86b48a53</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2022</creationdate><topic>Canyons</topic><topic>Civil Engineering</topic><topic>Climate change</topic><topic>Climate models</topic><topic>Design</topic><topic>Design floods</topic><topic>Downstream</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Environmental Management</topic><topic>Flood hydrographs</topic><topic>Flood peak</topic><topic>Floods</topic><topic>Future climates</topic><topic>Geophysics/Geodesy</topic><topic>Geotechnical Engineering & Applied Earth Sciences</topic><topic>Global climate</topic><topic>Global climate models</topic><topic>Hydrogeology</topic><topic>Hydrographs</topic><topic>Hydrologic processes</topic><topic>Hydrology</topic><topic>Natural Hazards</topic><topic>Original Paper</topic><topic>Precipitation anomalies</topic><topic>Probability theory</topic><topic>Reliability aspects</topic><topic>Reservoirs</topic><topic>Summer precipitation</topic><topic>Upstream</topic><topic>Water resources</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Li, Rongrong</creatorcontrib><creatorcontrib>Xiong, Lihua</creatorcontrib><creatorcontrib>Zha, Xini</creatorcontrib><creatorcontrib>Xiong, Bin</creatorcontrib><creatorcontrib>Liu, Han</creatorcontrib><creatorcontrib>Chen, Jie</creatorcontrib><creatorcontrib>Zeng, Ling</creatorcontrib><creatorcontrib>Li, Wenbin</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Environment 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Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Engineering collection</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>Environment Abstracts</collection><jtitle>Natural hazards (Dordrecht)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Li, Rongrong</au><au>Xiong, Lihua</au><au>Zha, Xini</au><au>Xiong, Bin</au><au>Liu, Han</au><au>Chen, Jie</au><au>Zeng, Ling</au><au>Li, Wenbin</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Impacts of climate and reservoirs on the downstream design flood hydrograph: a case study of Yichang Station</atitle><jtitle>Natural hazards (Dordrecht)</jtitle><stitle>Nat Hazards</stitle><date>2022-09-01</date><risdate>2022</risdate><volume>113</volume><issue>3</issue><spage>1803</spage><epage>1831</epage><pages>1803-1831</pages><issn>0921-030X</issn><eissn>1573-0840</eissn><abstract>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.</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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