My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
FLOOD09746
CWCB
>
Floodplain Documents
>
Backfile
>
9001-10000
>
FLOOD09746
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
1/26/2010 10:10:21 AM
Creation date
10/5/2006 4:37:09 AM
Metadata
Fields
Template:
Floodplain Documents
County
Statewide
Basin
Statewide
Title
Colorado Statewide Drainage Floodplain Management Criteria Manual
Date
8/1/2002
Prepared By
CWCB & WRC Engineering Inc
Floodplain - Doc Type
Educational/Technical/Reference Information
Jump to thumbnail
< previous set
next set >
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
310
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 />. <br /> <br /> <br />. <br /> <br />. <br /> <br />CHAPTER 5 <br />HYDROLOGY <br /> <br />SECTION 2.0 <br />RUNOFF <br /> <br />COLORADO STATEWIDE <br />DRAINAGE AND FLOODPLAIN MANAGEMENT CRITERIA MANUAL <br /> <br />2.2.1 METHODOLOGY <br /> <br />The Rational Formula method is based on the following equation: <br /> <br />Q=CIA <br /> <br />(Eq. CH5-200) <br /> <br />Q is defined as the maximum rate of runoff in cubic feet per second (actually, <br />Q has units of acre inches per hour, which is approximately equal to the units <br />of cubic feet per second). C is a runoff coefficient and represents the runoff- <br />producing conditions of the subject land area. I is the average intensity of <br />rainfall in inches per hour for a duration equal to the time of concentration. A <br />is the contributing basin area in acres. The time of concentration is defined <br />as the time required for water to flow from the hydraulically most distant part <br />of the drainage area to the point under consideration. <br /> <br />2.2.2 ASSUMPTIONS <br /> <br />The basic assumptions made when applying the Rational Formula method <br />are as follows: <br /> <br />1. The computed maximum rate of runoff to the design point is a <br />function of the average rainfall rate during the time of concentration to <br />that point. <br /> <br />2. The maximum rate of rainfall occurs during the time of concentration, <br />and the design rainfall depth during the time of concentration is <br />converted to the average rainfall intensity for the time of <br />concentration. <br /> <br />3. The maximum runoff rate occurs when the entire area is contributing <br />flow. However, this assumption has been modified from time to time <br />when local rainfall/runoff data was used to improve calculated results. <br /> <br />2.2.3 LIMITATIONS ON METHODOLOGY <br /> <br />The Rational Formula method can adequately <br />approximate the peak rate of runoff from a rainstonn in <br />a given small basin. The critics of the method usually <br />are unsatisfied with the fact that the answers are only <br />approximations. A shortcoming of the Rational Fonnula <br />method is that only one point on the runoff hydrograph <br />is computed (the peak runoff rate), therefore, the <br />estimated total runoff volume using the triangular <br />hydrograph is not very accurate. <br /> <br />2.2.4 TIME OF CONCENTRATION - RATIONAL METHOD <br /> <br />As previously mentioned, the time of concentration is <br />defined as the time required for runoff to flow from the <br />hydraulically most distant part of the drainage basin to <br />the desired point in the basin. <br /> <br />AUGUST 2002 <br /> <br />RUNOFF <br /> <br />The time of <br />concentration <br />is defined as <br />the time <br />required for <br />runoff to flow <br />from the <br />hydraulically <br />most distant <br />part of the <br />drainage <br />basin to the <br />desired point <br />in the basin. <br /> <br />CH5-204 <br />
The URL can be used to link to this page
Your browser does not support the video tag.