My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
FLOOD00925
CWCB
>
Floodplain Documents
>
Backfile
>
1-1000
>
FLOOD00925
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
11/23/2009 10:51:24 AM
Creation date
10/4/2006 9:35:57 PM
Metadata
Fields
Template:
Floodplain Documents
County
Statewide
Community
State of Colorado
Title
Colorado Flood Hydrology Manual - Section 22 Program
Date
9/1/1993
Prepared For
CWCB
Prepared By
US Army Corps of Engineers
Floodplain - Doc Type
Educational/Technical/Reference Information
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
133
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
Show annotations
View images
View plain text
<br />Where: <br /> <br />S = channel storage <br />K = cell travel time <br />X = weighting factor <br />I = inflow <br />o = outflow <br /> <br />Therefore, the coefficients can be expressed as follows: <br /> <br />(28) <br /> <br />(29) <br /> <br />(30) <br /> <br />(31) <br /> <br />(32) <br /> <br />In the Muskingum equation the amount of diffusion is based on the value <br />of X, which varies between 0.0 and 0.5. The Muskingum X parameter is not directly <br />related to physical channel properties. The diffusion obtained with the Muskingum <br />technique is a function of how the equation, is solved, and is therefore considered <br />numerical diffusion rather than physical. Cunge evaluated the diffusion that is <br />produced in the Muskingum equation and analytically solved for the following diffusion <br />coefficient: <br /> <br />(33) <br /> <br />In the Muskingum-Cunge formulation, the amount of diffusion is <br />controlled by forcing the numerical diffusion to match the physical diffusion <br />represented by the convective diffusion equation (23). this is accomplished by setting <br />equations (25) and (33) equal to each other. the Muskingum-Cunge equation is <br />therefore considered an approximation of the convective diffusion equation (23). As <br /> <br />7-52 <br />
The URL can be used to link to this page
Your browser does not support the video tag.