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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 />TABLE 6 (cont'd) <br />SUB-BASIN PARAMETERS FOR BIG DRY CREEK ANALYSIS <br /> <br /> Developed Loss Ra tes <br /> Drainage Length Ia Ia <br /> Sub-Basin Area L Lca % Impervious % Impervious * Ct Pervious Impervious Ini tia 1 Final <br />Flooding Source Designa tion (Sq. Mi.) (Mi) (Mi) Exis ting Developed Prog. Cp Retention Retention in/hr in/hr Decay Rate Comments <br />S. Hylands Creek 456 1.59 2.38 1.00 39.00 39.00 0.32 0.54 0.3 0.1 3.5 0.53 .0018 <br /> 457 2.17 3.33 1.76 34.50 40.80 0.37 0.60 0.4 0.1 3.4 0.53 .0018 includes 457 <br /> 454 0.02 0.38 0.19 5.00 54.50 0.19 0.37 0.4 0.1 3.0 0.50 .0018 <br />Middle Hylands C . 461 0.02 0.24 0.14 5.00 49.80 0.11 0.35 0.4 0.1 3.7 0.55 .0018 <br /> 460 0.71 1. 76 1.05 35.50 38.50 0.25 0.48 0.4 0.1 3.7 0.55 .0018 includes 461 <br /> 458 0.07 0.57 0.29 10.80 32.50 0.16 0.29 0.4 0.1 3.7 0.55 .0018 <br />N. Hylands Creek 463 0.08 0.38 0.29 30.30 43.00 0.13 0.38 0.4 0.1 3.7 0.55 .0018 <br /> 462 0.49 1.57 1.05 2.15 46.20 0.23 0.53 0.4 0.1 3.7 0.55 .0018 includes 463 <br />Walnu t Creek 672 5.00 5.71 2.19 34.10 34.10 0.36 0.56 0.4 0.1 3.1 0.51 .0018 <br /> 671 0.51 1.14 0.67 12.50 20.50 0.24 0.29 0.4 0.1 3.0 0.51 .0018 <br /> 670 0.22 1.14 0.62 5.00 33.80 0.30 0.35 0.4 0.1 3.1 0.51 .0018 <br /> 668 0.72 1.90 1.19 13.90 61.20 0.24 0.67 0.4 0.1 3.1 0.51 .0018 <br /> 676 0.65 2.19 1.05 9.30 9.30 0.39 0.27 0.4 0.1 3.0 0.50 .0018 <br /> 675 0.42 2.14 1.14 25.10 49.60 0.26 0.54 0.4 0.1 3.2 0.51 .0018 <br /> 663 0.19 0.76 0.38 16.80 46.40 0.18 0.46 0.4 0.1 3.6 0.54 .0018 <br /> 662 0.28 1.48 0.67 14.80 67.50 0.19 0.61 0.4 0.1 3.8 0.56 .0018 <br /> . 660 0.27 1.14 0.68 16.80 45.30 0.28 0.48 0.4 0.1 3.7 0.55 .0018 <br />Countryside Cr. 667 0.17 1.14 0.48 34.10 57.90 0.16 0.53 0.4 0.1 3.1 0.51 .0018 <br /> 666 0.43 0.86 0.57 24.40 48.60 0.19 0.54 0.4 0.1 3.0 0.50 .0018 <br /> 665 0.33 1.38 0.71 24.40 42.50 0.27 0.50 0.4 0.1 3.1 0.51 .0018 <br />N. Walnut Cr. 674 0.62 1.57 0.48 5.00 5.00 0.31 0.29 0.4 0.1 3.0 0.50 .0018 <br /> 673 1.14 3.86 1.05 5.80 15.10 0.36 0.30 0.4 0.1 3.1 0.51 .0018 includes 674 <br />Ketner Lake** 567 0.39 0.95 0.57 35.20 54.50 0.18 0.58 0.4 0.1 3.0 0.50 .0018 <br /> 566 0.22 0.95 0.43 24.00 46.10 0.20 0.47 0.4 0.1 3.1 0.51 .0018 <br />Ranch Creek** 216 0.11 0.43 0.24 38.80 80.00 0.12 0.57 0.4 0.1 3.0 0.05 .0018 <br /> 215 0.69 1.34 0.67 39.20 60.00 0.20 0.66 0.4 0.1 3.1 0.51 .0018 includes 216 <br /> 213 0.59 1.04 0.76 24.80 53.60 0.22 0.60 0.3 0.1 3.6 0.54 .0018 <br />S. Ranch Creek** 218 0.42 1.09 0.57 32.90 41.00 0.20 0.47 0.4 0.1 3.4 0.53 .0018 <br /> 217 0.70 1.52 0.76 26.90 42.50 0.23 0.52 0.4 0.1 3.4 0.53 .0018 includes 218 <br /> <br />* Ct adjusted for CUHP-D computer program for application of the 1982 version of the Colorado Urban Hydrograph Procedure <br /> <br />** Floodplain not delineated in this study - hydrology only <br /> <br />UNIT HYDROGRAPH EQUATIONS (CUHP-D <br /> <br />Ct (LLca) 0.18 <br />Ct (program) = <br />SoO.24 <br /> <br />Applica tion) <br />Tp = 60tp + 0.5 t" <br />Qp = qpA <br /> <br />in which, <br />A = drainage area of basin (in sq. mi.) <br />L = hydraulic length of basin in (miles) <br />Lca= centroidal length of basin in (miles) <br />So = average stream slope in (ft/ft) <br />Ct = unit hydrograph coefficient reflecting <br />time to peak (Figure 4-2) <br />peaking parameter related to I <br />percent impervious of basin a <br /> <br />C = <br />p <br /> <br /> 0.15 <br />Cp = PCtA <br />tp Ct (LLca) 0.3 <br />qp 640 cp/tp <br /> <br />tp= <br />qp= <br /> <br />unit hydrograph coefficient reflecting <br />peak discharge <br />time to peak of unit hydrograph in <br />(cfs/sq. mi.) <br />unit peak of unit hydrograph in <br />(cis/sq. mi.) <br />time of unit rainfall duration (min) <br />time to peak of unit hydrograph (min) <br />peak discharge of unit hydrograph (cfs) <br /> <br />7 <br /> <br />p = <br />I = <br />a <br /> <br />t = <br />u <br />T = <br />QP= <br />P <br /> <br />