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<br />6. COLORADO URBAN HYDROGRAPH PROCEDURE (CUHP) (From Yiessrnan, Lewis, <br />Knapp) <br /> <br />The Colorado Urban Hydrograph Procedure provides 5-minule synthetic unit <br />hydrographs for use in the Denver metropolitan area. It is based on Snyder's method and <br />is considered applicable to watersheds in the size range from 90 acres to 10 square miles, <br />with "regular" shapes (length = 4 times width). it was developed in the early 1980s and <br />modified in 1984 to reflect refinements from early applications. In its pre-1984 form, the <br />Synder/cUHP C, and Cp values are: <br /> <br />Ct - 7.81 <br />- p~.7li <br /> <br />(IY-15) <br /> <br />Cp = 0.89 C,O.46 <br /> <br />(IY-16) <br /> <br />Where p. is the percent imperviousness. These regression equations were developed for <br />p. > 30%, using data for 96 storms over 19 IJrban watersheds. The given equations apply <br />to normal watersheds conditions and need to be adjusted for steep, flat, or sewered <br />basins. If an urban area is fully sewered, the calculated C, from Eq. (IY-15) is decreased <br />10%. If sparsely sewered, a 10% increase is made. If the average slope, S of the lower <br />80% of the main water course is flat (less than 0.01 Wit) the C, value becomes: <br /> <br />C, <br /> <br />3.12 <br />p~. 78 SO.2 <br /> <br />(IY-17) <br /> <br />and for steep areas (S>0.025 ftIft): <br /> <br />C, <br /> <br />3. 75 <br />F"'.; 78 So. 2 <br /> <br />(IY-18) <br /> <br />The Cp coefficient is determined from Eq. (IY-16) and adjusted to 10% up or down for fully <br />or sparsely sewered conditions, respectively. <br /> <br />For CUHP applications equations for widths of the unit hydrograph are: <br /> <br />l-\o = 500 A <br />Qp <br /> <br />(IY-19) <br /> <br />Colorado Flood <br />Hydrology Manual <br /> <br />7-44 <br /> <br />a=w=r <br />