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Last modified
1/25/2010 6:48:24 PM
Creation date
10/5/2006 1:17:17 AM
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Template:
Floodplain Documents
County
Statewide
Community
State of Colorado
Basin
Statewide
Title
Urban Storm Drainage Criteria Manual
Date
5/1/1984
Prepared By
UDFCD
Floodplain - Doc Type
Flood Mitigation/Flood Warning/Watershed Restoration
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<br />DRAINAGE CRITERIA MANUAL <br /> <br />. <br /> <br />Step 9. <br /> <br />. <br /> <br />Step 10. <br /> <br />Step 11. <br />Step 12. <br /> <br />. <br /> <br />Step 13. <br /> <br />5-1-84 <br /> <br />RUNOFF <br /> <br />W75% ahead of Q = 0.45 x 11.2 <br />P <br />= 5.0 minutes <br /> <br />*Note: Less than 0.6 T = 9.6 minute; therefore <br />p <br />use 7.4 minutes and 5.0 minutes at W50% <br />and W75% respectively. If the 7.4 minutes <br />were greater than 0.6 T , the alternate <br />p <br />procedure would have been used. <br />Sketch the unit hydrograph (Figure 4-6) using Tp' Qp' W50%, <br />W75% and the portions of W50% and W75% ahead of Qp determined <br />above. <br />Needed Unit Hydrograph Volume: <br />(243 acres) x (1 inch/12 inch/foot) = 20.2 ac. ft. <br />Pl animeter the uni t hydrograph to obta in its volume. Adjust <br />recession leg of the hydrograph until 20.2 ac. ft. (:t5%) is <br />obtained. Volume of the first trial was 17.2 ac. ft. which is <br />15% to low. The unit hydrograph was revised as shown in Figure <br />4-6 and a volume of 20.3 ac. ft. was measured which is within <br />the required 5% accuracy. <br />Obtain the design effective precipitation values for from a <br />table similar to Table 2-5. To illustrate the process of <br />calculating a storm hydrograph, we will use in this example the <br />Effective Precipitation from Table 2-5 even though it was <br />calculated using a different value of imperviousness than is <br />used in this example. <br />Set up Table 4-1. <br />Multiply the precipitation value at the top of Column 3 by each <br />of the unit hydrograph ordinates and put in Column 3 for the <br />corresponding time. Next multiply the precipitation value in <br />Column 4 by each of the unit hydrograph ordinates and place in <br />col umn 4 lagged by one time increment from the corresponding <br />unit hydrograph time. Proceed to multiply each of the <br />precipitation values times the unit hydrograph ordinates, each <br />time lagging the new hydrograph by one more time unit. <br />Column 25 is the design storm hydrograph obtained by summing <br />horizontally the individual hydrographs in Column 3 through 24. <br />Note that in this example, time zero is the beginning of excess <br />
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