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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />In addition to the recorded data frequency statistics, the REGFREQ program also produces a set of <br />adopted frequency statistics. The adopted frequency statistics are created using smoothing functions built <br />into the program combined with the reconstituted frequency statistics to produce a smoothed set of <br />frequency statistics for the family of curves. The REGFREQ adopted frequency statistics were used <br />during the smoothing process as a guide, but not used outright. When the adopted statistics were plotted <br />along with the gage data, the fit was not found to provide an adequate fit in all cases. Two additional <br />guides used in the smoothing process were plotting standard deviation and skew values against the <br />mean for the family of curves. These plots were used to aid in the creation of a consistent trend in the <br />standard deviation and skew throughout the family of curves. This methodology is further described in <br />Chapter 3 of "Hydrologic Frequency Analysis - EM-111 0-2-1415" (USACE, 1993). The smoothed statistics <br />were estimated, plotted, and inspected for consistency and adjusted until a consistent set of curves was <br />developed that described the raw data for each individual member curve of the family. <br /> <br />The analytical distribution is only applicable for natural or unregulated peak flow data. The Taylor <br />Reservoir on the Taylor River has influenced the flow records for the Taylor River and Gunnison River <br />since construction in 1935 (Reaches 6,9, Taylor at A1mont, and Taylor below Taylor Park Reservoir). <br />Therefore, it is necessary to remove the influence of the reservoir from the regulated data set to generate <br />the unregulated flow data prior to performing the frequency analysis. Table 4.2.1 summarizes this <br />information for all reaches. <br /> <br />10 <br />