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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 />

9.4.3 User Notes<br />

9.4.3.1 Clark Unit Hydrograph<br />

1. The Clark Unit Hydrograph procedure was developed from a database that included<br />

both urban and natural (undeveloped) desert/rangeland watersheds. The primary<br />

application <strong>of</strong> the Clark Unit Hydrograph is for urban watersheds, but it is also applicable<br />

for undeveloped desert/rangeland watersheds. In general, the Clark Unit Hydrograph<br />

is not applicable to agricultural fields or steep mountain watersheds.<br />

2. The following limitations apply to the Clark Unit Hydrograph procedure.<br />

a. The recommended drainage area limit is 5 square miles with a maximum <strong>of</strong> 10<br />

square miles.<br />

b. The calculated T c should not exceed the duration <strong>of</strong> rainfall excess.<br />

c. The calculated T c should not be longer than 1.5 hours.<br />

If a drainage basin does not meet any or all <strong>of</strong> the preceding limitations, then the following<br />

options are available:<br />

• Subdivide the drainage area into smaller subbasins such that all <strong>of</strong> these subbasins<br />

satisfy the limitations.<br />

• Use the S-Graph method, provided the drainage basin satisfies the limitations<br />

<strong>of</strong> that method.<br />

• Justify the use <strong>of</strong> an alternative approach.<br />

3. Time <strong>of</strong> concentration as defined in this manual is the travel time, during the corresponding<br />

period <strong>of</strong> the most intense portion <strong>of</strong> rainfall excess, for a floodwave to<br />

travel from the hydraulically most distant point in the watershed to the point <strong>of</strong> interest.<br />

The determination <strong>of</strong> the hydraulically most distant point is made in regard to both<br />

length and slope. In other words, the hydraulically most distant point is not necessarily<br />

the longest length, but may be a shorter length with an appreciably flatter slope.<br />

4. When calculating the T c for a natural watershed, with slopes greater than 200 ft/mile,<br />

use Figure 5.4 to adjust the slope. The use <strong>of</strong> the adjusted slope should be considered<br />

when determining the T c <strong>of</strong> the hydraulically most distant point.<br />

5. T c is a function <strong>of</strong> rainfall excess and must be recalculated for each desired frequency<br />

or design storm duration.<br />

August 15, 2013 9-45

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