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<br />I <br />I <br />I <br /> <br />I <br />I <br /> <br />I <br />I <br />I <br />I <br /> <br />I <br />I <br />I <br /> <br />I <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />This was done to account for the fact that a large portion of the flow at the Gunnison near Gunnison gage <br />is unregulated flow contributed by the East River and Ohio Creek. However, the contribution from the <br />change in storage is better represented by the ratio determined for the gage closer to the reservoir. <br />Multiplying both the change in storage flow and the regulated flow by 1.0687 yields results significantly <br />lower than the results for the upstream reach, Gunnison River from Almont to Ohio Creek; therefore, the <br />alternative procedure is implemented for this study. For both gages, the estimated travel time from the <br />reservoir to the gage is less than 12 hours. Therefore, a lag is not applied. <br /> <br />5.0 INDIVIDUAL REACHES <br /> <br />The eight reaches, for which the peak flow analysis is desired, are analyzed. In addition, two more <br />reaches are included on the Taylor River since their results are needed to support the analysis of several <br />of the eight study reaches. Two of the eight reaches had sufficient stream gage data to warrant an <br />analysis based on the stream gage data alone. The other six study reaches and the two additional <br />reaches are altered or supplemented with nearby streamgage data. The characteristics, streamgage <br />information, correlation information, and results of analysis are presented below for each reach. <br /> <br />5.1 REACH 2 - SLATE RIVER TO CONFLUENCE WITH EAST RIVER <br /> <br />5.1.1 Description of Reach 2 <br /> <br />The Slate River reach extends from the confluence of the Slate River and the East River approximately <br />10 miles upstream to the confluence with Oh-Be-Joyful Creek with a drainage area of approximately 70 <br />square miles. Flows into the river are almost entirely from snowmelt runoff. <br /> <br />5.1.2 Flood Records for Reach 2 <br /> <br />There are reported peak flows from the USGS gage Slate River near Crested Butte for 1940 through <br />1951 and 1994 through 2000; however, a longer record would be more appropriate for completing an <br />analysis of flood flows in this reach. <br /> <br />The REGFREQ program was used to determine the correlation of the available flow data to nearby gages <br />on the Gunnison River system. A high degree of correlation (>0.9) between the Slate River gage and the <br />following gages were found. <br /> <br />· Taylor River at A1mont (09110000) <br />· East River at A1mont (09112500) <br />· East River below Cement Creek (09112200) <br />· Gunnison River near Gunnison (09114500) <br /> <br />The East River at Almont gage was chosen to expand the data set for the Slate River near Crested Butte <br />daily stream gage flows. The East River at Almont gage has a continuous record from 1935 through <br />2000. Although the other three gages noted above had slightly higher correlation, the East River gage <br />was chosen due to the longer available period of record and unprocessed results. The data from the <br />Taylor and Gunnison gages had been processed to remove the effects of the Taylor Park Reservoir. <br /> <br />No data are available for the upstream portions of the Slate River above the confluence with Coal Creek <br />and the town of Crested Butte. Data are available from Coal Creek for five years from 1941 through 1946. <br />These data indicate that from March through June, the contribution from Coal Creek is generally 10 to 20 <br />percent of the USGS recorded streamgage flow of the Slate River near Crested Butte. If flood flows were <br />needed for the portion of Slate Creek above Crested Butte, the results for the lower reach could be <br />reduced by 10 percent; or the results for the downstream reach could be used as a conservative value for <br /> <br />14 <br />