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<br />L "' length of the main stream channel (mi) from tile outlet <br />to the divide <br />Leo = length along tile main channel (mi) from the outlet <br />to a channel point nearest the watershed centroid <br /> <br />The peak rate and time of the unit hydrograph Can be developed using Eqs (IV-3) and (IV- <br />21). Alter four additional points defined by Eqs (IV-HI) and :IV-20) are plotted, tile rest of <br />the 5-min unit hydrograph can be fitted to provide a total area representing 1.0 incil of <br />direct runoff. A hand fit curve is applied to th" points. adjusting it to maintain trle proper <br />runoff volume. <br /> <br />For small watersheds (less tlan 90 acres), the time to peak is: <br /> <br />t p , C. 39 <br /> <br />(P~-0.3El Pa' 0.07) <br />------------- - . ---- <br />---------- <br />(P~. 0.49 Po '0.14) <br /> <br />(T, - 6 Pa) <br /> <br />(IV-23) <br /> <br />._iii <br /> <br />- <br /> <br />__iBm <br /> <br />Example 7.3 - Determine the storm hydrograph using the Colorado Urban Hydrogr3ph <br />Procedure (CUHP) and the fOllowing information. <br /> <br />Watershed Area = 0.38 square miles (243 acres) <br />Watershed Length = 1.28 miles <br />Distance to Centroid = 0.52 miles <br />Impervious Area = 44% <br />Slope along Watershed = 0.')102 It/lt <br /> <br />Excess precipitation in inches for 5 minutes intervals: <br />0.04 0.09 0.31 0.15 0.06 0.05 0.03 0.03 0.03 0.03 0.03 0.03 <br /> <br />Solution: <br /> <br />1. From Figure 1 - C, ~ 0.OD1 <br /> <br />2. tp = C, [(L L" IS)]"'" = (0.091)[(1.28)(0.52)/0.0102]048 = 0.225 hours ort3.5 rnin <br /> <br />3. From Figure 1 - Peaking ~arameter P ~ 6.21 <br />4. Cp = PC,Ao IS = (6.21 )(0.091 )(0.032-))0 '5 ~ 0.49 <br />5. qp = 640 Cp I tp = (El40)(0.49)/0.225 = 1394 Gfs I sq. mile <br />6. Op = qpA = (t,l94)(0.38) = 530 cfs <br /> <br />Colorado Flood <br />Hydrology Manual 7-46 <br /> <br />[R4/:T <br />