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<br />Peak flows along Rifle Creek were based on the regional regression <br />relationship and the routing of the inflow hydrograph through Rifle <br />Gap Reservoir. The hydrograph was developed from U.S. Soil Conser- <br />vation Service (SCS) methodology. The inflow peaks corresponded <br />to the peak as determined from the regression relationship, and <br />the volume was checked to correspond with the excess volume as <br />determined from the SCS analyses. <br /> <br />Peak discharge-drainage area relationships for the flooding sources <br />of the City of Rifle are shown in Table 1. <br /> <br />3.2 Hydraulic Analyses <br /> <br />Analyses of the hydraulic characteristics of flooding from the <br />sources studied were carried out to provide estimates of the eleva- <br />tions of floods of the selected recurrence intervals. <br /> <br />Water-surface elevations of floods of the selected recurrence inter- <br />vals were computed using the COE HEC-2 step-backwater program <br />(Reference 6). <br /> <br />Cross section data for the Colorado River were developed from <br />topographic maps furnished by the Colorado Department of Highways <br />(References 7 and 8). Cross sections for Rifle and Government <br />Creeks, and Hubbard Gulch were digitized from aerial photographs <br />flown in May 1980 (Reference 9). All bridges and culverts were <br />field surveyed to obtain elevation data and structural geometry. <br /> <br />Locations of selected cross sections used in the hydraulic analyses <br />are shown on the Flood Profiles (Exhibit 1). For stream segments <br />for which a flcodway was computed (Section 4.2), selected cross <br />section locations are also shown on the Flood Boundary and Floodway <br />Map (Exhibit 2). <br /> <br />Roughness factors (Manning's On") used in the hydraulic computations <br />were computed from stream gage data or determined by field obser- <br />vation using engineering judgment. Roughness values for the main <br />channel of the Colorado River ranged from 0.035 to 0.040, whereas <br />overbank roughness values ranged from 0.060 to 0.070. Roughness <br />values for the main channel of Rifle Creek ranged from 0.040 to <br />0.050, whereas overbank roughness values ranged from 0.050 to 0.080. <br />Roughness values for the main channel of Government Creek ranged <br />from 0.035 to 0.040, whereas overbank roughness values ranged from <br />0.035 to 0.045. Roughness values for the main channel of Hubbard <br />Gulch ranged from 0.035 to 0.045, whereas overbank roughness values <br />ranged from 0.035 to 0.050. <br /> <br />The starting water-surface elevations for the Colorado River, <br />Government Creek, and Hubbard Gulch were determined by the slope- <br />area method. The starting water-surface elevation for Rifle Creek <br />was taken as the normal depth for the given discharge. <br /> <br />7 <br />