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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>: Channel Routing<br />

7.4.1 Parameter Selection<br />

Application <strong>of</strong> Muskingum routing requires input values for parameters X and K. Parameter X<br />

has a range <strong>of</strong> values from 0.0 to 0.5, where 0.0 represents routing through a linear reservoir and<br />

0.5 indicates pure translation. Parameter K indicates the travel time <strong>of</strong> a floodwave through the<br />

entire routed reach. There are several methods which can be used to estimate K such as average<br />

flow velocity adjusted by a celerity factor, the time difference between peak inflow and peak<br />

outflow, or by using stage-discharge relationships. For more details the reader is referred to the<br />

HEC-1 manual and Section 9.5 <strong>of</strong> this manual. Once again, since the computational method<br />

within HEC-1 may result in an unstable solution, parameters K, X and NSTPS (number <strong>of</strong> steps)<br />

must be checked to insure that an adequate number <strong>of</strong> subreaches is used.<br />

In those rare situations that observed inflow and outflow hydrographs are available, K, X and<br />

NSTPS can be calibrated by trial and error to enable simulation <strong>of</strong> known outflow hydrographs.<br />

Chapter 5 <strong>of</strong> the USBR’s <strong>Flood</strong> <strong>Hydrology</strong> <strong>Manual</strong> (Cudworth, 1989) is an excellent source <strong>of</strong><br />

Muskingum routing information.<br />

7.5 MUSKINGUM-CUNGE ROUTING<br />

The Muskingum-Cunge routing method is based on the principle <strong>of</strong> hydraulic diffusivity, which<br />

simulates an attenuation <strong>of</strong> the flood peak through the routing reach. This method can be used<br />

for both man-made and natural channels where overbank flow is expected, provided the conveyance<br />

can be accurately described with an eight-point cross section. A complete description <strong>of</strong><br />

Muskingum-Cunge applications and guidelines for parameter selection can be found in the September<br />

1990 and later versions <strong>of</strong> the HEC-1 <strong>Flood</strong> Hydrograph Package User’s <strong>Manual</strong>.<br />

7.5.1 Parameter Selection<br />

Input data for Muskingum-Cunge routing include energy slope (or bed slope), reach length, and<br />

either the channel shape and a single Manning’s n for a man-made channel, or an eight-point<br />

cross section with channel and overbank roughness coefficients for a natural channel.<br />

7-4 August 15, 2013

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