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<br />I <br /> <br />I <br /> <br />I <br /> <br />I <br />I <br />I <br />I <br /> <br />I <br />I <br /> <br />I <br />I <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />The East River at A1mont gage was chosen to expand the data set for the Gunnison River near Gunnison <br />daily stream gage flows. The East River at Almont gage has a continuous record from 1935 through <br />2000. The East River gage was chosen since it had the highest degree of correlation, the longest <br />available period of record, and unprocessed results. Other gages had been processed to remove the <br />effects of the Taylor Park Reservoir. The resulting family of flow records is presented in Appendix A- <br />Table A.8. <br /> <br />Figure 5.8.2.1 Peak to Daily Flow Relationship - Gunnison River near Gunnison Gage <br />14,000 <br /> <br />~ 12,000 <br />~ <br />s::: <br />o <br />.~ <br />2 10,000 <br />::J <br />o <br /> <br /> <br />,; <br /> <br />. <br /> <br />... <br />:g 8,000 <br />s::: <br />s::: <br />o <br />.~ <br />s::: <br />s::: <br />::J <br />o <br /> <br />6,000 <br /> <br />III <br />:: 4,000 <br />o <br />u: <br />..\I: <br />11l <br />&. 2,000 <br /> <br />o <br />o <br /> <br />2,000 4,000 6,000 8,000 10,000 <br />Daily Peak Flows Gunnsion near Gunnison (cfs) <br /> <br />12,000 <br /> <br />5.8.3 Results for Reach 9 <br /> <br />Before any analysis was completed, the data record for both the East River at Almont and Gunnison <br />River near Gunnison gages were filtered for rain on snow events, using the 0.5 inch criteria discussed in <br />Section 4.1.1. Six rain on snow events were found in the record of the Gunnison River near Gunnison <br />gage. The East River at A1mont results are described in Section 5.4. <br /> <br />The REGFREQ and HEC-FFA programs were used to perform the analysis on the flow record in <br />Appendix A - Table A.8. Prior to using the REGFREQ program, HEC-FFA was used on both the East <br />River at Almont and Gunnison River near Gunnison data to test for low and high outliers based on a <br />methodology described in Bulletin 17B. Any outliers were manually removed from the REGFREQ data <br />set. The 1977 flow for the both gages was determined to be a low outlier. The results from the analysis <br />are presented in Figure 5.8.3.1. Additionally, the adopted statistics and the 10, 2, 1, and 0.2 percent <br />chance exceedence flows are presented in Table 5.8.3.1. <br /> <br />37 <br />