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<br />Rainfall <br />Rainfall data were obtained for the 10- and 100-year storms from the "Flood Hazard <br />Area Delineation (FHAD) - Broomfield Area" study by Wright-McLaughlin Engineers, <br />June 1979 (Reference 4). The rainfall data from this study had been developed <br />using Volume III of the NOAA "Precipitation-Frequency Atlas of the Western United <br />States" (Reference 5). The rainfall hyetographs for the various storm frequen- <br />cies are shown in Table 2. <br /> <br />.30 <br />.60 <br />.69 <br />.78 <br />1.32 <br />1.86 <br />3.24 <br />4.62 <br />2.97 <br />1.32 <br />1.05 <br />.78 <br />.63 <br />.48 <br />.39 <br />.30 <br />.27 <br />.24 <br />.24 <br />.24 <br />.21 <br />.18 <br />.18 <br />.18 <br /> <br />.48 <br />.96 <br />1.02 <br />1.08 <br />1.98 <br />2.88 <br />5.04 <br />7.20 <br />4.65 <br />2.10 <br />1.62 <br />1.14 <br />.81 <br />.48 <br />.42 <br />.36 <br />.33 <br />.30 <br />.30 <br />.30 <br />.30 <br />.30 <br />.28 <br />.24 <br /> <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 />HYDROLOGIC ANALYSES <br /> <br />TABLE 2 <br />QUAIL CREEK AND McKAY LAKE BASINS <br />RAINFALL HYETOGRAPHS (inches/hour) <br /> <br />Introduction <br />Hydrologic model 1 ing was used to develop the runoff estimates from the Quail <br />Creek and McKay Lake basins because historic stream flow measurements were not <br />available. The UDSWM2 program was used to determine the runoff hydrographs in <br />various conveyance elements along the drainageways. UDSWM2 (Reference 1) is the <br />name assigned by the Urban Drainage and Flood Control District (UDFCD) to the <br />Runoff Block of the Environmental Protection Agency's, Storm Water Management <br />Model (SWMM) program (Version 2) as modified by UDFCD and the Missouri River <br />Division of the U.S. Army Corps of Engineers (Reference 2). In an effort to make <br />the results of the UDSWM2 program more representative of rainfall/runoff data <br />collected within the UDFCD, the model was calibrated against the Colorado Urban <br />Hydrograph Procedure (CUHP) (Reference 3). Frequency discharges were developed <br />for each of the drainageways in this study for the 10- and 100-year storm events <br />using the UDSWM2 model. <br /> <br />UDSWM2 Model <br />The procedure for developing the mathematical abstraction of the actual drainage <br />basin is to divide the major basin into subcatchments that drain to conveyance <br />elements, then connect these conveyance elements to create a model of the drainage <br />system. Figure 1 shows the subcatchments, conveyance elements and various design <br />points for the Quail Creek and McKay Lake watersheds. <br /> <br />Time <br />(min) <br /> <br />5 <br />10 <br />15 <br />20 <br />25 <br />30 <br />35 <br />40 <br />45 <br />50 <br />55 <br />60 <br />65 <br />70 <br />75 <br />80 <br />85 <br />90 <br />95 <br />100 <br />105 <br />110 <br />115 <br />120 <br /> <br />10-Year <br /> <br />100-Year <br /> <br />The coefficients and parameters necessary to characterize hydraulic properties of <br />the subcatchment areas include the surface area, width, ground slope, roughness <br />coefficient, surface retention depth, infiltration rate, and percent impervious- <br />ness. The subcatchment parameters used for the Quail Creek basin are shown on <br /> <br />.. <br />