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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 />

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 />

5.7.2 S-Graph<br />

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

LL ca<br />

2. Calculate the basin factor<br />

0.5<br />

.<br />

S<br />

3. Using the data in Appendix D.1 or the tables in the <strong>Design</strong> <strong>of</strong> Small Dams or the<br />

USBR <strong>Flood</strong> <strong>Hydrology</strong> <strong>Manual</strong>, attempt to identify watersheds <strong>of</strong> the same physiographic<br />

type and similar drainage area and basin factor. Make a list <strong>of</strong> the watersheds<br />

with similar drainage areas and basin factors and tabulate the estimated value<br />

<strong>of</strong> K n for those watersheds and the measured lag.<br />

4. Estimate K n for the watershed by inspection <strong>of</strong> the tabulation from Step 3.<br />

5. Calculate the coefficient (C) and select the value <strong>of</strong> the exponent (m) corresponding to<br />

the source (Corps <strong>of</strong> Engineers or USBR) that was used to estimate K n . If the source<br />

<strong>of</strong> K n is unknown, then use the Corps <strong>of</strong> Engineers version <strong>of</strong> Equation (5.11).<br />

6. Using Equation (5.11), calculate the basin lag. Compare this value to the measured<br />

lags <strong>of</strong> watersheds from Step 3.<br />

7. Select an appropriate computational time interval (NMIN) and compute Q ult using<br />

Equation (5.10).<br />

8. Select an appropriate S-Graph and tabulate the percent Q ult , percent lag and the<br />

accumulated time.<br />

9. Transform the S-Graph into an X-duration (NMIN) unit hydrograph using linear interpolation<br />

with Δt = NMIN.<br />

10. Adjust the “tail” region <strong>of</strong> the S-Graph by lagging that portion by Δt and subtracting the<br />

ordinates.<br />

As an alternative to the above procedure, the DDMSW will transform the S-Graph to a<br />

unit graph automatically.<br />

August 15, 2013 5-31

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