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<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 />I <br />I <br /> <br />Chapter 4 <br />HYDROLOGY AND HYDRAULICS <br /> <br />Local flood hydrographs were developed for selected hydrologic <br />or pick-up points in each of the four basins. A flood hydro graph <br />measures total runoff, peak flow, and runoff distribution with <br />respect to time, the three most important parameters for <br />describing a flood event for a specific drainage basin. The <br />peak flow rate and runoff volume were determined for 2-year, <br />10-year, and 100-year storm frequencies. <br /> <br />As explained below in the "f1ydrology" section, each local <br />flood hydrograph was combined with the upstream flood hydrograph <br />and routed through upstream waterway crossings to allow for <br />flow backing up or impoundiAg at the crossings. The resulting <br />peak flow rate was used in ~he hydraulics analysis to determine <br />flood oepths and flood plaiA boundaries. This procedure is <br />discUS!iied in the "Hydraulic!>" section below. <br /> <br />The hyorographs are based oA each basin's existing level of <br />development and its total development as projected from the <br />planning maps of Arapahoe apd Jefferson Counties. Thus, the <br />flood bydrographs provide comparative data on existing land <br />use versus projected land u!iie ur.der the three flood frequencies. <br />Also, the results of the hyoraulics analysis, such as flood <br />water surface profiles and flood boundaries, are given for <br />both ezisting channel conditions and proposed channel improvements <br />based on a 100-year flood for a totally developeo basin. <br /> <br />HYDROLOGY <br /> <br />Each drainage basin was divided into subareas for study. The <br />subareas were determined from a field survey of tributary <br />collection points. The hydrologic or pick-up points associated <br />with each subarea are shown on Figure 3-2. Basin 6100 has <br />seven pick-up points (1-7 on Figure 3-2) and the North Tributary <br />to Basin 6200 has five pick-UP points (A-E on Fi~ure 3-2). <br /> <br />A single hydrograph was used for Direct Flow Basin 6100.5. <br />The pick-up point was at Platte Canyon Road and the culvert <br />250 feet north of Ken Caryl Road. A single hydrograph was <br />also set at the Platte Canyon Road crossing for the Downstream <br />Reach (Kiewit Area) of the Main Branch of Basin 6200. The <br />drainage area above this point is about 1,984 acres. The <br />hydrologic analyses for these two basins are discussed in <br />Chapters 7 and 8. <br /> <br />The local inflow flood hydrographs were developed from the <br />Colorado Urban Hydrograph Procedure (CUHP) as explained in <br />urban Storm Drainage Criteria Manual, March 1969, by Wright- <br />McLaughlin Engineers, distributed by the Urban Drainage and <br /> <br />4-1 <br />