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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 />

Table 5.3<br />

EQUATION FOR ESTIMATING K b IN THE T c EQUATION<br />

K b = m log A + b<br />

Where A is drainage area, in acres<br />

Equation<br />

Parameters<br />

Type Description Typical Applications<br />

m<br />

b<br />

A<br />

Minimal roughness: Relatively smooth<br />

and/or well graded and uniform land<br />

surfaces. Surfaces run<strong>of</strong>f is sheet<br />

flow.<br />

Commercial/industrial areas<br />

Residential area<br />

Parks and golf courses<br />

-0.00625 0.04<br />

B<br />

Moderately low roughness: Land<br />

surfaces have irregularly spaced<br />

roughness elements that protrude from<br />

the surface but the overall character <strong>of</strong><br />

the surface is relatively uniform.<br />

Surface run<strong>of</strong>f is predominately sheet<br />

flow around the roughness elements.<br />

Agricultural fields<br />

Pastures<br />

Desert rangelands<br />

Undeveloped urban lands<br />

-0.01375 0.08<br />

C<br />

Moderately high roughness: Land<br />

surfaces that have significant large to<br />

medium-sized roughness elements<br />

and/or poorly graded land surfaces<br />

that cause the flow to be diverted<br />

around the roughness elements.<br />

Surface run<strong>of</strong>f is sheet flow for short<br />

distances draining into meandering<br />

drainage paths.<br />

Hillslopes<br />

Brushy alluvial fans<br />

Hilly rangeland<br />

Disturbed land, mining, etc.<br />

Forests with underbrush<br />

-0.025 0.15<br />

D<br />

Maximum roughness: Rough land<br />

surfaces with tortuous flow paths. Surface<br />

run<strong>of</strong>f is concentrated in numerous<br />

short flow paths that are <strong>of</strong>ten<br />

oblique to the main flow<br />

direction.<br />

Mountains<br />

Some wetlands<br />

-0.030 0.20<br />

Note:<br />

A is the area <strong>of</strong> the entire subbasin, not the area <strong>of</strong> the surface type A, B, C or D within the<br />

subbasin.<br />

5.5.2 Storage Coefficient<br />

Very little literature exists on the estimation <strong>of</strong> the storage coefficient (R) for the Clark Unit Hydrograph.<br />

Clark (1945) had originally proposed a relation between T c and R since they can both be<br />

defined by locating the inflection point <strong>of</strong> a run<strong>of</strong>f hydrograph (refer to Figure 5.2). The Corps <strong>of</strong><br />

Engineers discuss the development <strong>of</strong> regionalized relations for T c and R as functions <strong>of</strong> watersheds<br />

characteristics in Training Document No. 15 (U.S. Army Corps <strong>of</strong> Engineers, 1982b).<br />

According to Corps procedures, T c and R are estimated from relations <strong>of</strong> T c + R and R / (T c + R)<br />

August 15, 2013 5-17

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