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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 />5.7 REACH 8 - TOMICHI CREEK FROM THE GUNNISON RIVER TO THE GUNNISON AIRPORT <br /> <br />5.7.1 Description of Reach 8 <br /> <br />. Reach 8 extends along T omichi Creek from the confluence with the Gunnison River approximately 2 <br />miles upstream, past the Gunnison Airport. The contributing drainage area is 1,061 square miles at the <br />downstream end of the reach and the entire reach length is unregulated. The reach is located just south <br />of the City of Gunnison and the Gunnison Airport. The watershed is primarily located in a high mountain <br />valley environment with elevations lower than the other reaches in this study. While annual peak <br />discharge values are primarily due to snowmelt runoff, the amount of snow pack in this watershed is <br />significantly less than the typical snow pack of the watersheds of the other reaches involved in this study. <br /> <br />This reach is located well below the significant snowmelt runoff sources; however, peak flows are still <br />primarily due to snowmelt runoff. The USGS gage Tomichi Creek at Gunnison (ID# 09119000) is located <br />along this reach and has a complete record of peak flows since 1938. <br /> <br />5.7.2 Flood Records for Reach 8 <br /> <br />The USGS gage Tomichi Creek at Gunnison includes peak flow data from 1938 through 2000. The <br />T omichi Creek at Gunnison gaged flows are representative of the flows along the entire Reach 8. The <br />reported family of flows for the USGS gage Tomichi Creek at Gunnison is presented in Appendix A- <br />Table A.7. <br /> <br />5.7.3 Results for Reach 8 <br /> <br />Before any analysis was completed, the data record for the Tomichi Creek gage was filtered for rain on <br />snow events, using the 0.5 inch criteria discussed in Section 4.1.1. Eight rain on snow events were found <br />in the record of the Tomichi Creek gage. <br /> <br />The REGFREQ and HEC-FFA programs were used to perform the analysis on the flow record in <br />Appendix A - Table A.7. Prior to using the REGFREQ program, HEC-FFA was used on Tomichi Creek to <br />test for low and high outliers based on a methodology described in Bulletin 17B. Any outliers were <br />manually removed from the REGFREQ data set. The 1984 was determined to be a high outlier. The <br />results from the analysis are presented in Figure 5.7.3,1. Additionally, the adopted statistics and the 10, 2, <br />1, and 0.2 percent chance exceedence flows are presented in Table 5.7.3.1. <br /> <br />33 <br />