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Deciphering Human Contributions to Yellow River Flow Reductions and Downstream Drying Using Centuries‐Long Tree Ring Records
The Yellow River flow has decreased substantially in recent decades, and the river often dried up in the lower reach and failed to reach the sea. Climate change and human disruption have been suggested as major causes of the flow reduction, but quantification of their relative contribution is challe...
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Published in: | Geophysical research letters 2019-01, Vol.46 (2), p.898-905 |
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container_title | Geophysical research letters |
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creator | Li, Jinbao Xie, Shang‐Ping Cook, Edward R. Chen, Fahu Shi, Jiangfeng Zhang, David D. Fang, Keyan Gou, Xiaohua Li, Teng Peng, Jianfeng Shi, Shiyuan Zhao, Yesi |
description | The Yellow River flow has decreased substantially in recent decades, and the river often dried up in the lower reach and failed to reach the sea. Climate change and human disruption have been suggested as major causes of the flow reduction, but quantification of their relative contribution is challenging due to limited instrumental records and disturbance by dams. Here we use a basin‐wide tree ring network to reconstruct the Yellow River flow for the past 1,200 years and show that the flow exhibits marked amplitude variations that are closely coupled to the hydrological mean state swings at multidecadal to centennial timescales. Recent flow should have increased to the highest level of the past 1,200 years if there were no human disruption. However, human activities have caused a loss of nearly half of natural flow since the late 1960s and are the main culprit for recent downstream flow reduction.
Plain Language Summary
Recent Yellow River flow reductions have had major impacts on China's economy and water policy. The short and heavily human‐modified gauge records are unable to reveal natural flow variability now and in the past. Here we use tree rings to reconstruct long‐term Yellow River flow, which enables an assessment of natural flow variability and the detection of human contributions to recent flow reductions. Our 1,200‐year reconstruction reveals that under natural conditions the Yellow River flow should have increased markedly since the early twentieth century. However, the observed flow decreased since the late 1960s and such a decrease must be predominately caused by human interventions instead of climate change.
Key Points
Human activities have drastically decreased Yellow River flow over the past decades
Recent Yellow River flow should have reached the highest level of the past 1,200 years if there were no human disruption
Anthropogenic flow reduction is estimated to be about 44.5% during 1969‐2010 |
doi_str_mv | 10.1029/2018GL081090 |
format | article |
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Plain Language Summary
Recent Yellow River flow reductions have had major impacts on China's economy and water policy. The short and heavily human‐modified gauge records are unable to reveal natural flow variability now and in the past. Here we use tree rings to reconstruct long‐term Yellow River flow, which enables an assessment of natural flow variability and the detection of human contributions to recent flow reductions. Our 1,200‐year reconstruction reveals that under natural conditions the Yellow River flow should have increased markedly since the early twentieth century. However, the observed flow decreased since the late 1960s and such a decrease must be predominately caused by human interventions instead of climate change.
Key Points
Human activities have drastically decreased Yellow River flow over the past decades
Recent Yellow River flow should have reached the highest level of the past 1,200 years if there were no human disruption
Anthropogenic flow reduction is estimated to be about 44.5% during 1969‐2010</description><identifier>ISSN: 0094-8276</identifier><identifier>EISSN: 1944-8007</identifier><identifier>DOI: 10.1029/2018GL081090</identifier><language>eng</language><publisher>Washington: John Wiley & Sons, Inc</publisher><subject>Climate change ; Detection ; Disruption ; Downstream ; Drying ; Hydrology ; Natural flow ; Records ; Reduction ; River flow ; Rivers ; Stream flow ; Tree rings ; Variability ; Water policies ; Water policy ; Yellow River flow</subject><ispartof>Geophysical research letters, 2019-01, Vol.46 (2), p.898-905</ispartof><rights>2018. American Geophysical Union. All Rights Reserved.</rights><rights>2019. American Geophysical Union. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a3679-cf50038e57ee3f2ff7cd7c227da259a76215e0c899b3dc1e9e63355c4e8d94703</citedby><cites>FETCH-LOGICAL-a3679-cf50038e57ee3f2ff7cd7c227da259a76215e0c899b3dc1e9e63355c4e8d94703</cites><orcidid>0000-0001-7478-4176 ; 0000-0001-7007-3983 ; 0000-0002-8919-4715 ; 0000-0002-3676-1325</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F2018GL081090$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2018GL081090$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,780,784,11513,27923,27924,46467,46891</link.rule.ids></links><search><creatorcontrib>Li, Jinbao</creatorcontrib><creatorcontrib>Xie, Shang‐Ping</creatorcontrib><creatorcontrib>Cook, Edward R.</creatorcontrib><creatorcontrib>Chen, Fahu</creatorcontrib><creatorcontrib>Shi, Jiangfeng</creatorcontrib><creatorcontrib>Zhang, David D.</creatorcontrib><creatorcontrib>Fang, Keyan</creatorcontrib><creatorcontrib>Gou, Xiaohua</creatorcontrib><creatorcontrib>Li, Teng</creatorcontrib><creatorcontrib>Peng, Jianfeng</creatorcontrib><creatorcontrib>Shi, Shiyuan</creatorcontrib><creatorcontrib>Zhao, Yesi</creatorcontrib><title>Deciphering Human Contributions to Yellow River Flow Reductions and Downstream Drying Using Centuries‐Long Tree Ring Records</title><title>Geophysical research letters</title><description>The Yellow River flow has decreased substantially in recent decades, and the river often dried up in the lower reach and failed to reach the sea. Climate change and human disruption have been suggested as major causes of the flow reduction, but quantification of their relative contribution is challenging due to limited instrumental records and disturbance by dams. Here we use a basin‐wide tree ring network to reconstruct the Yellow River flow for the past 1,200 years and show that the flow exhibits marked amplitude variations that are closely coupled to the hydrological mean state swings at multidecadal to centennial timescales. Recent flow should have increased to the highest level of the past 1,200 years if there were no human disruption. However, human activities have caused a loss of nearly half of natural flow since the late 1960s and are the main culprit for recent downstream flow reduction.
Plain Language Summary
Recent Yellow River flow reductions have had major impacts on China's economy and water policy. The short and heavily human‐modified gauge records are unable to reveal natural flow variability now and in the past. Here we use tree rings to reconstruct long‐term Yellow River flow, which enables an assessment of natural flow variability and the detection of human contributions to recent flow reductions. Our 1,200‐year reconstruction reveals that under natural conditions the Yellow River flow should have increased markedly since the early twentieth century. However, the observed flow decreased since the late 1960s and such a decrease must be predominately caused by human interventions instead of climate change.
Key Points
Human activities have drastically decreased Yellow River flow over the past decades
Recent Yellow River flow should have reached the highest level of the past 1,200 years if there were no human disruption
Anthropogenic flow reduction is estimated to be about 44.5% during 1969‐2010</description><subject>Climate change</subject><subject>Detection</subject><subject>Disruption</subject><subject>Downstream</subject><subject>Drying</subject><subject>Hydrology</subject><subject>Natural flow</subject><subject>Records</subject><subject>Reduction</subject><subject>River flow</subject><subject>Rivers</subject><subject>Stream flow</subject><subject>Tree rings</subject><subject>Variability</subject><subject>Water policies</subject><subject>Water policy</subject><subject>Yellow River flow</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2019</creationdate><recordtype>article</recordtype><recordid>eNp9kLFOwzAQhi0EEqWw8QCWWCmc7SS2R5TSFikSUtUOTFHqXCBVGhc7oeqCeASekSchJQxMLHe_7j79d_oJuWRww4DrWw5MTRNQDDQckQHTQTBSAPKYDAB0p7mMTsmZ92sAECDYgLyP0ZTbF3Rl_Uxn7SaraWzrxpWrtilt7Wlj6RNWld3RefmGjk5-JOat6fdZndOx3dW-cZht6NjtD05Lf6gx1k3rSvRfH5-J7QYLh9j5dGqOxrrcn5OTIqs8Xvz2IVlO7hfxbJQ8Th_iu2SUiUjqkSnC7mGFoUQUBS8KaXJpOJd5xkOdyYizEMEorVciNww1RkKEoQlQ5TqQIIbkqvfdOvvaom_StW1d3Z1MOZNaqIBz3VHXPWWc9d5hkW5ducncPmWQHhJO_ybc4bzHd2WF-3_ZdDpPQhUEWnwD-qd-jQ</recordid><startdate>20190128</startdate><enddate>20190128</enddate><creator>Li, Jinbao</creator><creator>Xie, Shang‐Ping</creator><creator>Cook, Edward R.</creator><creator>Chen, Fahu</creator><creator>Shi, Jiangfeng</creator><creator>Zhang, David D.</creator><creator>Fang, Keyan</creator><creator>Gou, Xiaohua</creator><creator>Li, Teng</creator><creator>Peng, Jianfeng</creator><creator>Shi, Shiyuan</creator><creator>Zhao, Yesi</creator><general>John Wiley & Sons, Inc</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7TN</scope><scope>8FD</scope><scope>F1W</scope><scope>FR3</scope><scope>H8D</scope><scope>H96</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>L7M</scope><orcidid>https://orcid.org/0000-0001-7478-4176</orcidid><orcidid>https://orcid.org/0000-0001-7007-3983</orcidid><orcidid>https://orcid.org/0000-0002-8919-4715</orcidid><orcidid>https://orcid.org/0000-0002-3676-1325</orcidid></search><sort><creationdate>20190128</creationdate><title>Deciphering Human Contributions to Yellow River Flow Reductions and Downstream Drying Using Centuries‐Long Tree Ring Records</title><author>Li, Jinbao ; Xie, Shang‐Ping ; Cook, Edward R. ; Chen, Fahu ; Shi, Jiangfeng ; Zhang, David D. ; Fang, Keyan ; Gou, Xiaohua ; Li, Teng ; Peng, Jianfeng ; Shi, Shiyuan ; Zhao, Yesi</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a3679-cf50038e57ee3f2ff7cd7c227da259a76215e0c899b3dc1e9e63355c4e8d94703</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2019</creationdate><topic>Climate change</topic><topic>Detection</topic><topic>Disruption</topic><topic>Downstream</topic><topic>Drying</topic><topic>Hydrology</topic><topic>Natural flow</topic><topic>Records</topic><topic>Reduction</topic><topic>River flow</topic><topic>Rivers</topic><topic>Stream flow</topic><topic>Tree rings</topic><topic>Variability</topic><topic>Water policies</topic><topic>Water policy</topic><topic>Yellow River flow</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Li, Jinbao</creatorcontrib><creatorcontrib>Xie, Shang‐Ping</creatorcontrib><creatorcontrib>Cook, Edward R.</creatorcontrib><creatorcontrib>Chen, Fahu</creatorcontrib><creatorcontrib>Shi, Jiangfeng</creatorcontrib><creatorcontrib>Zhang, David D.</creatorcontrib><creatorcontrib>Fang, Keyan</creatorcontrib><creatorcontrib>Gou, Xiaohua</creatorcontrib><creatorcontrib>Li, Teng</creatorcontrib><creatorcontrib>Peng, Jianfeng</creatorcontrib><creatorcontrib>Shi, Shiyuan</creatorcontrib><creatorcontrib>Zhao, Yesi</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Technology Research Database</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Geophysical research letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Li, Jinbao</au><au>Xie, Shang‐Ping</au><au>Cook, Edward R.</au><au>Chen, Fahu</au><au>Shi, Jiangfeng</au><au>Zhang, David D.</au><au>Fang, Keyan</au><au>Gou, Xiaohua</au><au>Li, Teng</au><au>Peng, Jianfeng</au><au>Shi, Shiyuan</au><au>Zhao, Yesi</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Deciphering Human Contributions to Yellow River Flow Reductions and Downstream Drying Using Centuries‐Long Tree Ring Records</atitle><jtitle>Geophysical research letters</jtitle><date>2019-01-28</date><risdate>2019</risdate><volume>46</volume><issue>2</issue><spage>898</spage><epage>905</epage><pages>898-905</pages><issn>0094-8276</issn><eissn>1944-8007</eissn><abstract>The Yellow River flow has decreased substantially in recent decades, and the river often dried up in the lower reach and failed to reach the sea. Climate change and human disruption have been suggested as major causes of the flow reduction, but quantification of their relative contribution is challenging due to limited instrumental records and disturbance by dams. Here we use a basin‐wide tree ring network to reconstruct the Yellow River flow for the past 1,200 years and show that the flow exhibits marked amplitude variations that are closely coupled to the hydrological mean state swings at multidecadal to centennial timescales. Recent flow should have increased to the highest level of the past 1,200 years if there were no human disruption. However, human activities have caused a loss of nearly half of natural flow since the late 1960s and are the main culprit for recent downstream flow reduction.
Plain Language Summary
Recent Yellow River flow reductions have had major impacts on China's economy and water policy. The short and heavily human‐modified gauge records are unable to reveal natural flow variability now and in the past. Here we use tree rings to reconstruct long‐term Yellow River flow, which enables an assessment of natural flow variability and the detection of human contributions to recent flow reductions. Our 1,200‐year reconstruction reveals that under natural conditions the Yellow River flow should have increased markedly since the early twentieth century. However, the observed flow decreased since the late 1960s and such a decrease must be predominately caused by human interventions instead of climate change.
Key Points
Human activities have drastically decreased Yellow River flow over the past decades
Recent Yellow River flow should have reached the highest level of the past 1,200 years if there were no human disruption
Anthropogenic flow reduction is estimated to be about 44.5% during 1969‐2010</abstract><cop>Washington</cop><pub>John Wiley & Sons, Inc</pub><doi>10.1029/2018GL081090</doi><tpages>8</tpages><orcidid>https://orcid.org/0000-0001-7478-4176</orcidid><orcidid>https://orcid.org/0000-0001-7007-3983</orcidid><orcidid>https://orcid.org/0000-0002-8919-4715</orcidid><orcidid>https://orcid.org/0000-0002-3676-1325</orcidid><oa>free_for_read</oa></addata></record> |
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issn | 0094-8276 1944-8007 |
language | eng |
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source | Wiley Online Library AGU 2017 |
subjects | Climate change Detection Disruption Downstream Drying Hydrology Natural flow Records Reduction River flow Rivers Stream flow Tree rings Variability Water policies Water policy Yellow River flow |
title | Deciphering Human Contributions to Yellow River Flow Reductions and Downstream Drying Using Centuries‐Long Tree Ring Records |
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