My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
PUB00083
CWCB
>
Publications
>
Backfile
>
PUB00083
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/11/2009 11:41:28 AM
Creation date
9/30/2006 10:14:56 PM
Metadata
Fields
Template:
Publications
Year
1997
Title
Historical Dry and Wet Periods in Colorado (Draft Copy)
CWCB Section
Water Conservation & Drought Planning
Author
McKee, Doesken, Kleist
Description
Analysis tool used to describe both drought and wet events for periods in Colorado.
Publications - Doc Type
Tech Report
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
109
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 />6.0 Summary and Conclusions <br />A study to document the drought (dry) and wet periods in Colorado during this century <br />has been conducted using precipitation, snowpack and streamflow observations. Drought and <br />wet periods have been defined using the Standardized Precipitation Index (SPI) for a variety of <br />time scales including 3, 6, 12, 24 and 48 months. A range of time scales are used since the time <br /> <br />for precipitation to be transformed to water sources of soil moisture, snowpack, streamflow, <br /> <br />reservoir water, and ground water vary. The 3-6 month periods are more related to snowpack <br /> <br />and soil moisture. Time scale of6-12 months have more relationship to streamflow and reservoir <br /> <br />water which the 24-48 month time scale is related to reservoir water, streamflow and <br /> <br /> <br />groundwater. A fundamental character of precipitation is that the longer the averaging period the <br /> <br /> <br />less impact a short time period has on accumulated precipitation. Consequently, the longer time <br /> <br /> <br />scales (averaging periods) have fewer dry and wet periods but the periods last longer. In the U.S. <br /> <br /> <br />the 3 month time scale leads to approximately 65 drought periods in 100 years with an average <br /> <br /> <br />duration of 6 months. A time scale of 24 months is needed to reduce the number of droughts to <br /> <br /> <br />about 10 per 100 years with a duration of nearly 13 months. Thus the frequency of drought (wet) <br /> <br />periods, the duration, and the magnitude of precipitation deficit are all a function of the time scale. <br /> <br />Severity of drought and wet periods are not affected by time scale. <br /> <br />An analysis of the fraction ofpreciptiation observing sites in dry or wet conditions <br /> <br />indicates that approximately 60% of the state can be dry or wet at the 24 month time scale. Using <br /> <br />the percentage of sites being dry or wet, the dry and wet periods this century are: <br /> <br />26 <br />
The URL can be used to link to this page
Your browser does not support the video tag.