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<br />- <br />14 <br /> <br />Improving American River Flood Frequency Analyses <br /> <br /> <br />of the sample and regional skews, as suggested in Bulletin 17-B. No historical data <br />were used in the analysis, reportedly because it did not appear that use of historical <br />data would affect the results. Finally, the expected probability adjus1ment was applied <br />to the estimated distributions. The three-day flow values computed by the USACE <br />(1998) were 215,000 cubic feet per second (cfs) for the roO-year flood and 278,000 <br />cfs for the 200-year flood at the Fair Oaks gage. For perspective, estimates of the <br />three-day flow values for the 1986 and 1997 floods at Fair Oaks are 166,000 cfs and <br />164,250 cfs, respectively. <br /> <br />Reactions to USACE Analysis <br /> <br />The methods and results of the USACE flood frequency analysis have <br />prompted several questions, comments, and criticisms from representatives of local, <br />state, and federal govemment agencies, public interest groups, private citizens, as well <br />as from the Corps itself. These concerns were conveyed to the committee both orally <br />and in writing over the course of this study. In addition, the committee identified <br />other issues of concern. Below is a list of the issues that the committee recognized as <br />potentially critical, and that are addressed in this report: <br /> <br />. accuracy of the adjusted daily flows used in the flood frequency analysis; <br />. failure of the USACE analysis to incorporate historical data or paleoflood <br />information; . <br />. consistency of the results with probable maximum flood estimates, <br />envelope curves of maximum flood discharges, and rainfall nmoff modeling results; <br />. use of the Bulletin l7-B map skew, given that the skew map is out of date <br />and was developed for instantaneous flood discharges, not maximum daily flows; <br />. the use of the expected probability correction; <br />. adequacy of the log-Pearson type ill distribution for modeling flood <br />distributions over a wide range of exceedance probabilities; <br />. adequacy of the Bulletin 17-B procedure for accounting for historical data; <br />. the potential advantages of censoring the lower part of the distribution so <br />that the estimation depends only on the largest floods; <br />. the fact that the record from 1950 to the present has many more large <br />floods than the 1905-1950 record; and <br />. potential changes in flood probability due to global climate or regional <br /> <br />change. <br /> <br />The first two issues concern data used (or not used) in the USACE analysis, <br />and are discussed in Chapter 2. The next six issues concern methods of flood <br />frequency analysis, and are discussed in Chapter 3. The last two issues concern <br />climate and its bearing on the standard assumption that flood discharges are <br />independent and identically distributed in time; this is the focus of Chapter 4. <br />In evaluating the issues of data, analysis methods, and climate, the committee <br />strictly adhered to scientific standards. Hence, each technical recommendation, <br />presented in Chapter 5, is based on best judgment of what is consistent with the <br />scientific literature. It is important, however, to recognize the following: <br /> <br />. Estimations of flood quantiles and probabilities are based on a number of <br />