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Drainage Design Manual, Hydrology - Flood Control District of ...

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<strong>Drainage</strong> <strong>Design</strong> <strong>Manual</strong> for Maricopa County<br />

<strong>Hydrology</strong>: Application<br />

9.4 UNIT HYDROGRAPH<br />

9.4.1 Procedures for the Clark Unit Hydrograph<br />

1. From an appropriate map <strong>of</strong> the watershed, measure drainage area (A) and the values<br />

<strong>of</strong> L and S.<br />

2. If S is greater than 200 ft/mi, adjust the slope using Table 5.2 or Figure 5.4.<br />

3. Using Figure 5.5 and Table 5.3, select a resistance coefficient (K b ) for the basin or<br />

subbasin based on a resistance classification and the drainage area (in acres). For a<br />

basin or subbasin <strong>of</strong> mixed classification;<br />

• A representative K b can be interpolated from Figure 5.5, or<br />

• An arithmetically averaged K b can be calculated based on the area <strong>of</strong> each<br />

unique K b present in the basin or subbasin.<br />

4. Calculate T c as a function <strong>of</strong> i using Equation (5.5)<br />

5. Enter the following data into an HEC-1 input file:<br />

• <strong>Design</strong> rainfall per the methodology and procedures in Chapter 2;<br />

• Basin area;<br />

• Rainfall loss data per the methodologies and procedures in Chapter 4; and<br />

• Clark unit hydrograph parameters (values set to zero).<br />

6. Run HEC-1 with the input file from Step 5 at an output level <strong>of</strong> zero for each subbasin.<br />

Rank the incremental rainfall excess values from smallest to highest for each subbasin<br />

and sum the ten (10) highest values. Compute the average rainfall intensity, i, by<br />

dividing the sum by the total <strong>of</strong> ten (10) computation time intervals and convert to units<br />

<strong>of</strong> hours (total <strong>of</strong> 10 highest rainfall excess values/(10(NMIN/60)).<br />

7. Compute T c using the equation from Step 4 above.<br />

8. Calculate R using Equation (5.8).<br />

9. Select the appropriate time-area relation for the basin or subbasin.<br />

As an alternative to the above procedures, the DDMSW program will compute the rainfall<br />

excess directly and perform the necessary iterations to compute the T c and R parameters.<br />

August 15, 2013 9-43

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