My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
PROJ00441
CWCB
>
Loan Projects
>
Backfile
>
1-1000
>
PROJ00441
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
11/19/2009 11:43:25 AM
Creation date
10/5/2006 11:55:35 PM
Metadata
Fields
Template:
Loan Projects
Contract/PO #
C153459
Contractor Name
Loveland, City of
Water District
0
County
Larimer
Bill Number
XB 99-999
Loan Projects - Doc Type
Feasibility Study
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
113
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 />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />o Duration (in months) <br /> <br />o Probability of occurrence <br /> <br />o Amount of water available during the drought (or magnitude of <br />defie! ts) <br /> <br />The probability of occurrence can be stated as a "recurrence interval" of a <br /> <br /> <br />specified time period. The recurrence interval is the average amount of <br /> <br /> <br />time between droughts of similar duration and water availability. A <br /> <br /> <br />drought with a lO-year recurrence interval would occur, on average, once <br /> <br /> <br />during any ten year period. <br /> <br />In the past, the reliability of a water supply system was usually <br />determined by comparing the monthly demands on the system to the flow <br />available for a specific drought; this drought was then referred to as the <br />"design" drought. The design drought may have been selected from historic <br />droughts experienced in the region or estimated from statistical analysis <br />of available streamflow or precipitation data. The choice of which <br />particular drought of all drought possibilities to use as the design <br />drought was based on a combination of hydrologic and non-technical factors <br />such as: <br /> <br />o The frequency and severity of water supply shortages experienced in <br />the pas t. <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />o The frequency of large variations in streamflow. <br /> <br />o Policy decisions, i.e., a City may decide to protect against a <br />certain drought event as a matter of policy. <br /> <br />o The availability of alternate sources of supply during drought <br />conditions. <br /> <br />Recent advances in computers has allowed the use of statistical and <br /> <br /> <br />stochastic techniques to supplement the analysis of historic data. These <br /> <br /> <br />techniques are used to generate a long-term (several hundred or thousand <br /> <br /> <br />years) record of "synthetic" streamflow. These synthetic streamflow <br /> <br /> <br />histories maintain the monthly, seasonal, and annual characteristics of the <br /> <br />2-3 <br />
The URL can be used to link to this page
Your browser does not support the video tag.