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<br />t. <br /> <br />I <br />I <br />I <br />I <br />I <br />I' <br />I <br />I <br /> <br /> <br />, <br /> <br />I <br /> <br /> <br />! <br /> <br /> <br />I <br />I <br />I; <br /> <br /> <br />. <br /> <br />It <br />I: <br />I, <br />I. - <br />I <br />Ii: <br />IL <br /> <br />Having estimated the magnitude of flood peaks on the Gunnison <br />River, a comparison of the flood hydrographs for the Colorado and <br />Gunnison Rivers was made to determine when the peaks occurred. <br /> <br />Figures 4, 5, and 6 show hydrographs during the high .flow years <br />of 1957, 1962, and 1984. It can be assumed that flood peaks on <br />the Colorado and Gunnison Rivers occur at the same time since <br />these hydrographs are nearly parallel. <br /> <br />Thus, for study reaches downstream of the mouth of the Gunnison, <br />the peak discharges on the Colorado are added to the flood peaks <br />computed for the Gunnison. <br /> <br />Thus, the proposed de sign discharges on the Colorado River study <br />reach are as follows: <br /> 10-yr 50-yr 100-yr 500-yr <br />study area above mouth 32,900 44,400 49,300 61,000 <br />of Gunnison <br />study area below mouth 50,600 73,100 83,700 111,400 <br />of Gunnison <br /> <br />The previous FISs used the peak discharges listed in the <br />following table. <br /> <br />Previous FISs 10-Yr 50-yr 100-yr 500-yr <br />study area above mouth 40,000 56,400 63,000 82,000 <br />of Gunnison <br />Study area below mouth 55,000 73,000 82,000 107,000 <br />of Gunnison <br /> <br />B. Big Salt Wash and Little Salt Wash <br /> <br />The Flood Hazard Information Report for Fruita, 1976 (3), <br />discusses the hydrologic studies conducted by the Sacramento <br />District of the Corps of Engineers on Big Salt Wash and Little <br />Sal t Wash. Because streamflow gauging information was not <br />available for these two streams, the Corps derived unit <br />hydrographs by the S-graph method, based on an S-graph developed <br />for Rifle Creek at Rifle. A standard project storm was developed <br />for the washes from a compilation of precipitation records. <br />Using frequency curves developed for other regional drainage <br />basins similar in size to the study area drainages, ratios of <br />100-year and 500-year floods to the standard project flood were <br />determined. These peak discharges developed by the Corps will be <br />used in the on-going studies also. The 1976 hydrologic studies <br />also developed information on 10-year and 50-year flood events <br />but the design discharges are not listed in the report. <br /> <br />-8- <br /> <br />