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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 />TABLE 4.1 PEAK FLOWS FOR RETURN PERIODS ON THE GUNNISON RIVER AT DELTA. CO <br /> <br />Return Periods FIS Delta, CO <br />(years) AUQ. 19, 1991 <br />10 13,500 <br />50 18,700 <br />100 21,200 <br />500 26,700 <br /> <br />4.2 Diversions and Returns <br />There are no significant diversions between the Delta gage and the Hartland diversion. <br />However, there are two ditches, which return to the Gunnison River immediately upstream of <br />the gage. These ditches are the Relief canal and Bona Fide ditch. The returns are not <br />monitored but are believed to return up to 20 to 30 cfs (Boyd 2000). For the purpose of this <br />analysis these returns are considered negligible. <br /> <br />4.3 Average Monthly Flows <br />Using gage information from 1976 through the end of 1999, the daily minimum, mean, <br />and maximum flows are calculated for each month. Exceedences for mean daily flows are also <br />determined. As previously discussed, April through August is the critical time for fish passage. <br />Results of the gage analysis are presented in Table 4.2. <br />Based on the analysis, the average spring runoff since 1976 occurs in late Mayor early <br />June. 30 days prior to the peak, average flows are approximately 3000 cfs. Average daily <br />flows in August are approximately 1200 cfs with a 50% exceedence of 1100 cfs. The 90% <br />exceedence for August is 350 cfs. <br />Flood flow-frequency curves for the Gunnison River are based on gage information <br />using log-Pearson Type III distribution for events that are not available from the FIS (USWRC <br />1981). These return periods and flows are presented in Table 4.3. <br /> <br />14 <br />