Socio-economic Impacts on Flooding: A 4000-Year History of the Yellow River, China
We analyze 4000-year flood history of the lower Yellow River and the history of agricultural development in the middle river by investigating historical writings and quantitative time series data of environmental changes in the river basin. Flood dynamics are characterized by positive feedback loops...
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Veröffentlicht in: | Ambio 2012-11, Vol.41 (7), p.682-698 |
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description | We analyze 4000-year flood history of the lower Yellow River and the history of agricultural development in the middle river by investigating historical writings and quantitative time series data of environmental changes in the river basin. Flood dynamics are characterized by positive feedback loops, critical thresholds of natural processes, and abrupt transitions caused by socio-economic factors. Technological and organizational innovations were dominant driving forces of the flood history. The popularization of iron plows and embankment of the lower river in the 4th century BC initiated a positive feedback loop on levee breaches. The strength of the feedback loop was enhanced by farming of coarse-sediment producing areas, steep hillslope cultivation, and a new river management paradigm, and finally pushed the flood frequency to its climax in the seventeenth century. The co-evolution of river dynamics and Chinese society is remarkable, especially farming and soil erosion in the middle river, and central authority and river management in the lower river. |
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M ; Gao, Shu ; Overeem, Irina ; Kettner, Albert J</creator><creatorcontrib>Chen, Yunzhen ; Syvitski, James P. M ; Gao, Shu ; Overeem, Irina ; Kettner, Albert J</creatorcontrib><description>We analyze 4000-year flood history of the lower Yellow River and the history of agricultural development in the middle river by investigating historical writings and quantitative time series data of environmental changes in the river basin. Flood dynamics are characterized by positive feedback loops, critical thresholds of natural processes, and abrupt transitions caused by socio-economic factors. Technological and organizational innovations were dominant driving forces of the flood history. The popularization of iron plows and embankment of the lower river in the 4th century BC initiated a positive feedback loop on levee breaches. The strength of the feedback loop was enhanced by farming of coarse-sediment producing areas, steep hillslope cultivation, and a new river management paradigm, and finally pushed the flood frequency to its climax in the seventeenth century. The co-evolution of river dynamics and Chinese society is remarkable, especially farming and soil erosion in the middle river, and central authority and river management in the lower river.</description><identifier>ISSN: 0044-7447</identifier><identifier>EISSN: 1654-7209</identifier><identifier>DOI: 10.1007/s13280-012-0290-5</identifier><identifier>PMID: 22673799</identifier><language>eng</language><publisher>Dordrecht: Springer-Verlag</publisher><subject>17th century ; 4th century ; Agricultural development ; Agricultural history ; Agricultural production ; Atmospheric Sciences ; Avulsions ; China ; Cities ; coevolution ; Community supported agriculture ; Earth and Environmental Science ; Ecology ; Economic factors ; Economic impact ; Economics ; Environment ; Environmental changes ; Environmental Engineering/Biotechnology ; Environmental Management ; Farming ; Feedback ; Flood frequency ; Flood irrigation ; Floods ; Fluvial channels ; Fluvial erosion ; History ; Levees ; Levees & battures ; Loess ; Natural channels ; new technology ; Physical Geography ; plows ; Precipitation ; REVIEW PAPER ; River basins ; Rivers ; Sediment transport ; Sedimentation & deposition ; Sediments ; society ; Socioeconomic Factors ; Socioeconomics ; Soil erosion ; technology ; Time series ; time series analysis ; watersheds ; Yellow River</subject><ispartof>Ambio, 2012-11, Vol.41 (7), p.682-698</ispartof><rights>2012 Royal Swedish Academy of Sciences</rights><rights>Royal Swedish Academy of Sciences 2012</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-b637t-472afbd45cd64fb88cf79580b6342e23b4bf1c6345f358731b1ccadc6d4fe6563</citedby><cites>FETCH-LOGICAL-b637t-472afbd45cd64fb88cf79580b6342e23b4bf1c6345f358731b1ccadc6d4fe6563</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/23322893$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/23322893$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>230,314,723,776,780,799,881,27901,27902,41464,42533,51294,53766,53768,57992,58225</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/22673799$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Chen, Yunzhen</creatorcontrib><creatorcontrib>Syvitski, James P. M</creatorcontrib><creatorcontrib>Gao, Shu</creatorcontrib><creatorcontrib>Overeem, Irina</creatorcontrib><creatorcontrib>Kettner, Albert J</creatorcontrib><title>Socio-economic Impacts on Flooding: A 4000-Year History of the Yellow River, China</title><title>Ambio</title><addtitle>AMBIO</addtitle><addtitle>Ambio</addtitle><description>We analyze 4000-year flood history of the lower Yellow River and the history of agricultural development in the middle river by investigating historical writings and quantitative time series data of environmental changes in the river basin. Flood dynamics are characterized by positive feedback loops, critical thresholds of natural processes, and abrupt transitions caused by socio-economic factors. Technological and organizational innovations were dominant driving forces of the flood history. The popularization of iron plows and embankment of the lower river in the 4th century BC initiated a positive feedback loop on levee breaches. The strength of the feedback loop was enhanced by farming of coarse-sediment producing areas, steep hillslope cultivation, and a new river management paradigm, and finally pushed the flood frequency to its climax in the seventeenth century. The co-evolution of river dynamics and Chinese society is remarkable, especially farming and soil erosion in the middle river, and central authority and river management in the lower river.</description><subject>17th century</subject><subject>4th century</subject><subject>Agricultural development</subject><subject>Agricultural history</subject><subject>Agricultural production</subject><subject>Atmospheric Sciences</subject><subject>Avulsions</subject><subject>China</subject><subject>Cities</subject><subject>coevolution</subject><subject>Community supported agriculture</subject><subject>Earth and Environmental Science</subject><subject>Ecology</subject><subject>Economic factors</subject><subject>Economic impact</subject><subject>Economics</subject><subject>Environment</subject><subject>Environmental changes</subject><subject>Environmental Engineering/Biotechnology</subject><subject>Environmental Management</subject><subject>Farming</subject><subject>Feedback</subject><subject>Flood frequency</subject><subject>Flood irrigation</subject><subject>Floods</subject><subject>Fluvial channels</subject><subject>Fluvial erosion</subject><subject>History</subject><subject>Levees</subject><subject>Levees & battures</subject><subject>Loess</subject><subject>Natural channels</subject><subject>new technology</subject><subject>Physical Geography</subject><subject>plows</subject><subject>Precipitation</subject><subject>REVIEW PAPER</subject><subject>River basins</subject><subject>Rivers</subject><subject>Sediment transport</subject><subject>Sedimentation & deposition</subject><subject>Sediments</subject><subject>society</subject><subject>Socioeconomic Factors</subject><subject>Socioeconomics</subject><subject>Soil erosion</subject><subject>technology</subject><subject>Time series</subject><subject>time series analysis</subject><subject>watersheds</subject><subject>Yellow River</subject><issn>0044-7447</issn><issn>1654-7209</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><sourceid>EIF</sourceid><sourceid>8G5</sourceid><sourceid>BENPR</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNqFkk9vFCEYxonR2G31A3hQSbx4EOU_Mx5Mmo21TZqYtPbQE2EY2GUzM2xhtqbfvkyn1upBT0Ce3_u88D4A8IrgjwRj9SkTRiuMMKEI0xoj8QQsiBQcKYrrp2CBMS97ztUe2M95gzGWjLHnYI9SqZiq6wU4O482RORsHGIfLDzpt8aOGcYBHnUxtmFYfYaHkJdadOlMgschjzHdwOjhuHbw0nVd_AnPwrVLH-ByHQbzAjzzpsvu5f16AC6Ovv5YHqPT799OloenqJFMjYgranzTcmFbyX1TVdarWlS4qJw6yhreeGLLQXgmKsVIQ6w1rZUt904KyQ7Al9l3u2t611o3jMl0eptCb9KNjiboP5UhrPUqXmtWWmMiisH7e4MUr3Yuj7oP2ZYHmcHFXdYFqbmgpfv_UULKSJW8Q9_9hW7iLg1lEncUYapEVygyUzbFnJPzD_cmWE_h6jlcXcLVU7h6uu-bxw9-qPiVZgHoDOQiDSuXHrX-h-vruWgzBfvblDFKq5oV_e2sexO1WaWQ9cV5md_0JaTCkrNbYKO_xg</recordid><startdate>20121101</startdate><enddate>20121101</enddate><creator>Chen, Yunzhen</creator><creator>Syvitski, James P. 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Technological and organizational innovations were dominant driving forces of the flood history. The popularization of iron plows and embankment of the lower river in the 4th century BC initiated a positive feedback loop on levee breaches. The strength of the feedback loop was enhanced by farming of coarse-sediment producing areas, steep hillslope cultivation, and a new river management paradigm, and finally pushed the flood frequency to its climax in the seventeenth century. The co-evolution of river dynamics and Chinese society is remarkable, especially farming and soil erosion in the middle river, and central authority and river management in the lower river.</abstract><cop>Dordrecht</cop><pub>Springer-Verlag</pub><pmid>22673799</pmid><doi>10.1007/s13280-012-0290-5</doi><tpages>17</tpages><oa>free_for_read</oa></addata></record> |
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subjects | 17th century 4th century Agricultural development Agricultural history Agricultural production Atmospheric Sciences Avulsions China Cities coevolution Community supported agriculture Earth and Environmental Science Ecology Economic factors Economic impact Economics Environment Environmental changes Environmental Engineering/Biotechnology Environmental Management Farming Feedback Flood frequency Flood irrigation Floods Fluvial channels Fluvial erosion History Levees Levees & battures Loess Natural channels new technology Physical Geography plows Precipitation REVIEW PAPER River basins Rivers Sediment transport Sedimentation & deposition Sediments society Socioeconomic Factors Socioeconomics Soil erosion technology Time series time series analysis watersheds Yellow River |
title | Socio-economic Impacts on Flooding: A 4000-Year History of the Yellow River, China |
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