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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 />I <br />. <br />I <br /> <br />which wallowed in the muddy waters pushing fill into the rapidly <br />disappearing banks. The bridge was saved, though a portion of a <br />city tile sewer line adjacent to the bank was carried away in the <br />flood." <br /> <br />- HYDROLOGY AND HYDRAULIC DETERMINATIONS - <br /> <br />Hydrologic Analysis <br /> <br />Hydrologic analysis of the Tucker Gulch and Kenneys Run drainage basins were <br />performed to determine peak discharges and flood hydrographs at selected <br />critical points along the studied streams. Flood discharges were determined <br />for the 10-, 50- and 100-year rainfall events assuming future developed basin <br />conditions. Table I shows the peak flow rates selected for hydraulic model- <br />ling. <br /> <br />"Another famil i ar source of fl oodi ng in Gol den was Kinney Run. a <br />gulch which drains part of Lookout Mountain and comes through Golden <br />into Clear Creek. The relentless rain was too much for the most <br />often dry gulch, and its waters spilled over onto Golden Road at a <br />point next to the Lookout Mountain School for Boys. The water <br />there joined with another torrent from south Table Mountain and <br />closed down Ford and Jackson Streets for part of the day. <br /> <br />Many homes in the area, particularly around Ford and Jackson at <br />21st, were badly hit by the rising waters, their basements filling <br />up like bathtubs." <br /> <br />Tucker Gulch: The hydrologic analysis for the Tucker Gulch drainage basin <br />involved dividing the basin into five sub-basins and utilizing the Colorado <br />Urban Hydrograph Procedure (CUHP) to determine runoff hydrographs from each <br />sub-basin. The hydrographs were combined and routed down stream channels <br />using the Convex Routing Method. The resulting flood hydrographs were used <br />to select the peak discharges for hydraulic modelling. Figure 1 shows the <br />basin and sub-basin boundaries; Figure 2 shows the discharge probability <br />profiles. and Figure 3 shows typical 100-year flood hydrographs. <br /> <br />The preceding are examples of some of the most damaging floods experienced in <br />Golden. It should be noted that many other floods have also inflicted damage. <br />Although only one newspaper article was found regarding flooding on Kenneys <br />Run, local sources noted that the storm sewers commonly became plugged, <br />forcing floodwaters down Jackson and Ford Streets. <br /> <br />The basin and unit hydrograph parameters are tabulated in Table II. The <br />procedure used to determine the CUHP parameters is outlined in the Urban Drainage <br />and Flood Control District's Urban Storm Drainage Criteria Manual. Recent <br />modifications were applied to the procedure as recommended by the Urban Drainage <br />and Flood Control District. The modified CUHP equations are listed following <br />Table II. Detailed documentation of the hydrologic analysis is available at <br />the office of the Urban Drainage and Flood Control District. <br /> <br />One-hour point rainfall depths were determined from the Precipitation-Frequency <br />Atlas of the Western United States, NOAA Atlas 2, Vol. III, Colorado, 1973, <br />for the 2-, 5-, 10-, 50- and 100-hear return periods. These values were used <br />to develop the two-hour design storms based upon a time distribution of rainfall <br />recommended by Urban Drai nage and Fl ood Control Di strict. Areal reducti ons of <br /> <br />8 <br />