My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
WSP03063
CWCB
>
Water Supply Protection
>
Backfile
>
3001-4000
>
WSP03063
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
1/26/2010 12:48:27 PM
Creation date
10/11/2006 11:31:16 PM
Metadata
Fields
Template:
Water Supply Protection
File Number
8449.900
Description
Bear Creek
State
CO
Basin
South Platte
Date
1/1/1980
Author
CWCB
Title
Board Memos and Resolutions
Water Supply Pro - Doc Type
Board Memo
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
64
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 />.' <br /> <br />MROED-HE <br />SUBJECT: <br /> <br />(1 Jul 82) <br />Evaluation of Potential Water Supply Storage at Chatfield Reservoir in <br />Colorado <br /> <br />TO: Chief, Planning Div FROM: Chief, Engrg Diy DATE: 29 Sep 82 CMT 112 <br /> <br />1. We have completed our preliminary reevaluation of the Reservoir Design Floods <br />on Cherry Creek, Bear Creek and Chatfield. These reevaluation studies were based <br />on providing enough storage at each project to control the standard project rainfall <br />flood or the SOO-year snowmelt flood using the original design release criteria. A <br />detailed outline of the studies that were made for all three projects is presented <br />in the following paragraphs. <br /> <br />,a. Cherry Creek. A standard project flood was deyeloped for the Cherry Creek <br />D~ study which was included in our studies of the Sand and Toll Gate Creek basins. <br />The total volume of this flood can be stored below spillway crest. However, the <br />adverse'emergency operating characteristics of this project make it a very unlikely <br />candidate for use as a water supply storage facility. In addition to the freeboard <br />being inadequate during a probable maximum flood event, the flood water is directed <br />into another watershed as soon as the pool level is higher than the spillway crest. <br /> <br />b. Chatfield. The Chatfield Reservoir Design Flood was selected by exaoining <br />"three conditions that can cause major flooding on the South Platte River at the <br />damsite. Based on a review of the design criteria used in developing each rainfall <br />flood condition it became apparent that the criteria in each case was more severe <br />than a standard project or a SOO-year snowmelt event. The following paragraphs <br />describe the amjustments that were made under each condition to change the level <br />of protection to the standards discussed at the outset. <br /> <br />(1) Condition ,1. A combination of the 1942 snowmelt flood, wbich was the <br />record spring flood in this region. and a May'standard project flood was the basic <br />assumption for this condition in the Chatfield Reservoir Design Flood. In our <br />ree aluation study we used a 10- ear s rin flood as the coincident event. It was <br />determined on a volume pro ability basis from the South Platte River gaging station <br />record at South Platte using April-May flows only in a 60-day analysis. This resulted <br />in a Chatfield coincident inflow volume of about 40% of the 1942 snowmelt flood. The <br />same S-day sbutdown period and stepped release rate used in the 'design studies was <br />used in the new operation of tbe standard project flood inflow. A comparison of the <br />old and new storage requirements is presented in table ~. <br /> <br />(2) Condition 2. This condition was based on a 1000-year spring inflow <br />coincident witb the rainfall runoff flood of record (June 1965). The reevaluation <br />study was based on a SOO-year sprinR inflow coincident with a May I-day, lu-year <br />event on Plum Creek at Louviers. Although our SOO-year ratio was only 1.63 times <br />the 1942 flood versus the design ratio of 1.7 for the 1000-year event, our distribu- <br />tion was more critical during the storage inflow period. Because our rainfall runoff <br />inflow was considerably less, the' shutdown period during, the flood operation was <br />reduced from S days to 2 days and the releases were stepped at 1000 cfs incr~ents <br />per day instead of the design SOO cfs, These results are also shown in the table <br />below. <br /> <br />2 <br />
The URL can be used to link to this page
Your browser does not support the video tag.