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Last modified
1/25/2010 6:46:09 PM
Creation date
10/5/2006 12:37:36 AM
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Floodplain Documents
County
Statewide
Basin
Statewide
Title
Improving American River Flood Frequency Analysis
Date
1/1/1999
Prepared By
National Research Council
Floodplain - Doc Type
Educational/Technical/Reference Information
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<br />Sacramento and the Struggle to Manage Flood Risk <br /> <br />- <br />13 <br /> <br /> <br />TECHNICAL ISSUES A.l'ID POLICY IMPLICATIONS <br /> <br />In FebruaI)' 1998, the USACE published a revised unregulated rain flood <br />flow frequency analysis for the American River at Fair Oaks (USACE, 1998)/ This <br />revision "''as the fIrst since 1986, and was motivated by the occurrences in 1986 and <br />1997 of two major floods on the American River. As expected, the analysis produced <br />a flood frequency curve that indicates that large floods are appreciably more likely <br />than previously thought Based on the newly estimated 100-year flood discharge, the <br />levees protecting Sacramento would no longer provide protection against the 100-year <br />flood according to criteria' set by the Federal Emergency Management Agency-the <br />effect of this essentially being "decertifIcation" of the existing levees to provide 100- <br />year protection and new requirements for the purchase of flood insurance. The <br />revised flow frequency relationships also reduce the estimated level of protection of <br />the flood control alternatives that are currently being considered for Sacramento. <br /> <br />USACE Approach <br /> <br />In calculating the revised flood frequency analysis, the USACE used daily <br />flow data collected at the Fair Oaks gage (USGS #11446500) that were adjusted for <br />the impact of upstream reservoirs.' The adjustment consisted of adding the gaged <br />mean daily flows to the daily change in storage at Folsom Lake and the lagged daily <br />change in storage of the most signifIcant reservoirs in the upper American River basin <br />(the latter accounting for about 90% of all storage in the upper basin). The change in <br />storage for the upstream reservoirs was lagged by one day to account for travel time. <br />For each year of record, the maximum rain-event flows for 1-, 3-, 5-, 7-, 10-, 15-, and <br />30-day durations were extracted (USACE, 1998). Spring snowmelt events were <br />excluded to avoid mixing populations. <br /> <br />Analyses <br /> <br />In conducting flood frequency analysis on each of the maxirnmn flow series, <br />the USACE was guided by Bulletin 17-B (IACWD, 1982). The mean, standard <br />deviation, and coefficient of skewness of the logarithm of the flow series were <br />computed from the flow series. (The 15-day and 30-day flows for 1977 were <br />identifIed as outliers; but in order to avoid having the frequency curves cross, the <br />flows were not censored.) Forthe I-day, 3-day, and 5-day series, the skews used were <br />weighted averages of the sample and regional skews; for the remaining durations, <br />sample skews were used directly. The regional skews were based on the skew map <br />given in Plate I of Bulletin 17-B, and weighting was based on the mean square errors <br /> <br />I Unregulated rain flood flow frequency analysis is conducted on annual peak flow <br />data that have been corrected for the effects of reservoir storage and are associated with <br />events that are primarily due to rainfall rather than snowmelt <br />] 44 CFR 65 of the Code of Federal Regulations. <br />j Daily rather than instantaneous flows are critical to flood management decision on <br />the American River because of the significant volume of upstream flood storage at <br />Folsom Dam. <br />
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