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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>: Unit Hydrograph Procedures<br />

5.7 PROCEDURES<br />

Procedures for calculating the unit hydrograph parameters are provided in the following sections.<br />

Notes and general guidance on the application <strong>of</strong> these procedures and the methodologies presented<br />

in this chapter are provided along with a detailed example in Section 9.4.4.<br />

5.7.1 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 either Figure 5.5 or Table 5.3, select a resistance coefficient (K b ) for the basin<br />

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

a 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 />

a. 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.<br />

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

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

From the HEC-1 output file, find the rainfall excess at each time interval.<br />

Rank the values from the highest to the lowest. The average rainfall intensity is<br />

found by summing up the first ten highest rainfall excess values and dividing the<br />

result by the length <strong>of</strong> ten time intervals.<br />

c. Directly solve Equation (5.5) for T c using the computed average rainfall intensity.<br />

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

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

5-30 August 15, 2013

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