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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 />I <br />I <br /> <br />to 75 square miles were applied to the 15-minute most intense period of the <br />design storms based on Area-Depth Curves developed by NOAA. Table I shows <br />typical design storms used for hydrologic modeling; these storms include <br />the area adjustment for a watershed between 50 and 75 square miles in area. <br /> <br />TABLE I <br />SIX-HOUR DESIGN STORMS <br />BIG DRY CREEK <br />AREAllY ADJUSTED FOR WATERSHEDS OF 50 TO 75 SQUARE MILES <br /> <br />The drainage sub-basin parameters used in the CUHP model are tabulated in <br />Table II. The procedure used to determine the CUHP parameters is outlined <br />in the Runoff Chapter of Reference 4. A schematic of the SWMM routing <br />network is shown in Figure 2. The 5WMM conveyance element parameters were <br />estimated based upon the project mapping and field observations and are <br />listed in Table III. Detailed documentation of the hydrologic analysis is <br />available at the office of the UDFCD. The following paragraphs contai,n <br />specific information regarding the hydrologic analysis. <br /> <br />- ext <br />f ~ f + (f. - f )e <br />o , 0 <br /> <br />Time (Min) <br /> <br />5 <br />10 <br />15 <br />20 <br />25 <br />30 <br />35 <br />40 <br />45 <br />50 to 75 <br />80 <br />85 to 115 <br />120 to 155 <br />160 to 360 <br /> <br />10-Year Design <br />Storm 5-min. <br />Rainfall Increments <br />(inches) <br /> <br />Time (Min) <br /> <br />100-Year Design <br />Storm 5-min. <br />Rainfall Increments <br />( inches) <br /> <br />where: <br /> <br />.03 <br />.07 <br />.14 <br />.16 <br />.26 <br />.12 <br />.09 <br />.08 <br />.07 <br />.06 <br />.04 <br />.03 <br />.02 <br />.01 <br /> <br />5 <br />10 <br />15 <br />20 <br />25 <br />30 <br />35 <br />40 <br />45 <br />50 <br />55 to 65 <br />70 to 75 <br />80 to 120 <br />125 to 190 <br />195 to 360 <br /> <br />.04 <br />.10 <br />.14 <br />.21 <br />.23 <br />.40 <br />.27 <br />.21 <br />.20 <br />.15 <br />.13 <br />.07 <br />.03 <br />.02 <br />.01 <br /> <br />Parameters to predict infiltration loss rates were estimated based on a <br />preliminary inventory of soils prepared by the U.S.D.A. Soil Conservation <br />Service (Reference 9). Infiltration losses were computed within the CUHP <br />model using Horton's Equation: <br /> <br />f ~ <br />f. ~ <br />, <br />fo ~ <br />ex ~ <br />t = <br /> <br />infiltration rate in inches/hour, <br />initial infiltration rate in inches/hour, <br />final infiltration rate in inches/hour, <br />decay coefficient in per second units, and <br />time in seconds. <br /> <br />TOTALS <br /> <br />2.20 <br /> <br />3.37 <br /> <br />Future land use in the tributary watershed was estimated usin9 planning <br />documents from Thornton, Broomfield, Westminster, and Adams County. This <br />information was then translated into future percent impervious land surface <br />area (I ) for the hydrology modeling, and is shown in Figure 1 and <br />a <br />summarized in Table IV. Values of I for each sub-basin are listed with <br />a <br />the other CUHP parameters in Table II. <br /> <br />5 <br />