Drought Analysis with Reservoirs Using Tree-Ring Reconstructed Flows
This paper presents a drought study of the Sacramento River of California considering the presence of reservoirs. A total of 508 years (1485-1992) of annual flow data are used. The data prior to 1872 was reconstructed from tree-ring data of Oregon and California using statistical and stochastic tech...
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Veröffentlicht in: | Journal of hydraulic engineering (New York, N.Y.) N.Y.), 1995-05, Vol.121 (5), p.413-421 |
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creator | Shen, Hsieh Wen Tabios III, Guillermo Q |
description | This paper presents a drought study of the Sacramento River of California considering the presence of reservoirs. A total of 508 years (1485-1992) of annual flow data are used. The data prior to 1872 was reconstructed from tree-ring data of Oregon and California using statistical and stochastic techniques. Runs analysis is used to investigate the drought characteristics for three cases: (1) No reservoir; (2) a reservoir with a myopic release rule; and (3) a reservoir with an anticipatory release rule. It is found that: (1) The tree-ring reconstructed flows in this study are better than a previous data reconstruction; (2) the reconstructed data showed that other severe droughts occurred prior to 1872, when historical records were available, thus there are risks involved in relying solely on the historical data; (3) the Sacramento River basin experienced the most severe droughts around the 1580s and 1930s; and (4) the results of the cases with reservoirs have significantly longer interarrival times between drought events, a much smaller number of drought events, and much less severe water shortages and cumulative deficits in contrast to the results with no reservoir. |
doi_str_mv | 10.1061/(ASCE)0733-9429(1995)121:5(413) |
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A total of 508 years (1485-1992) of annual flow data are used. The data prior to 1872 was reconstructed from tree-ring data of Oregon and California using statistical and stochastic techniques. Runs analysis is used to investigate the drought characteristics for three cases: (1) No reservoir; (2) a reservoir with a myopic release rule; and (3) a reservoir with an anticipatory release rule. It is found that: (1) The tree-ring reconstructed flows in this study are better than a previous data reconstruction; (2) the reconstructed data showed that other severe droughts occurred prior to 1872, when historical records were available, thus there are risks involved in relying solely on the historical data; (3) the Sacramento River basin experienced the most severe droughts around the 1580s and 1930s; and (4) the results of the cases with reservoirs have significantly longer interarrival times between drought events, a much smaller number of drought events, and much less severe water shortages and cumulative deficits in contrast to the results with no reservoir.</description><identifier>ISSN: 0733-9429</identifier><identifier>EISSN: 1943-7900</identifier><identifier>DOI: 10.1061/(ASCE)0733-9429(1995)121:5(413)</identifier><identifier>CODEN: JHEND8</identifier><language>eng</language><publisher>Reston, VA: American Society of Civil Engineers</publisher><subject>Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; Freshwater ; Hydrology. 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It is found that: (1) The tree-ring reconstructed flows in this study are better than a previous data reconstruction; (2) the reconstructed data showed that other severe droughts occurred prior to 1872, when historical records were available, thus there are risks involved in relying solely on the historical data; (3) the Sacramento River basin experienced the most severe droughts around the 1580s and 1930s; and (4) the results of the cases with reservoirs have significantly longer interarrival times between drought events, a much smaller number of drought events, and much less severe water shortages and cumulative deficits in contrast to the results with no reservoir.</description><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>Freshwater</subject><subject>Hydrology. 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Hydrogeology</topic><topic>TECHNICAL PAPERS</topic><topic>Water resources</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Shen, Hsieh Wen</creatorcontrib><creatorcontrib>Tabios III, Guillermo Q</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Aqualine</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Civil Engineering Abstracts</collection><jtitle>Journal of hydraulic engineering (New York, N.Y.)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Shen, Hsieh Wen</au><au>Tabios III, Guillermo Q</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Drought Analysis with Reservoirs Using Tree-Ring Reconstructed Flows</atitle><jtitle>Journal of hydraulic engineering (New York, N.Y.)</jtitle><date>1995-05-01</date><risdate>1995</risdate><volume>121</volume><issue>5</issue><spage>413</spage><epage>421</epage><pages>413-421</pages><issn>0733-9429</issn><eissn>1943-7900</eissn><coden>JHEND8</coden><abstract>This paper presents a drought study of the Sacramento River of California considering the presence of reservoirs. A total of 508 years (1485-1992) of annual flow data are used. The data prior to 1872 was reconstructed from tree-ring data of Oregon and California using statistical and stochastic techniques. Runs analysis is used to investigate the drought characteristics for three cases: (1) No reservoir; (2) a reservoir with a myopic release rule; and (3) a reservoir with an anticipatory release rule. It is found that: (1) The tree-ring reconstructed flows in this study are better than a previous data reconstruction; (2) the reconstructed data showed that other severe droughts occurred prior to 1872, when historical records were available, thus there are risks involved in relying solely on the historical data; (3) the Sacramento River basin experienced the most severe droughts around the 1580s and 1930s; and (4) the results of the cases with reservoirs have significantly longer interarrival times between drought events, a much smaller number of drought events, and much less severe water shortages and cumulative deficits in contrast to the results with no reservoir.</abstract><cop>Reston, VA</cop><pub>American Society of Civil Engineers</pub><doi>10.1061/(ASCE)0733-9429(1995)121:5(413)</doi><tpages>9</tpages></addata></record> |
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source | American Society of Civil Engineers:NESLI2:Journals:2014 |
subjects | Earth sciences Earth, ocean, space Exact sciences and technology Freshwater Hydrology. Hydrogeology TECHNICAL PAPERS Water resources |
title | Drought Analysis with Reservoirs Using Tree-Ring Reconstructed Flows |
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