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WSP02689
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WSP02689
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Last modified
7/29/2009 10:46:12 PM
Creation date
10/11/2006 11:17:52 PM
Metadata
Fields
Template:
Water Supply Protection
File Number
8040.970
Description
Basin Outlook Reports
State
CO
Date
1/1/1999
Author
USDOA
Title
Colorado Basin Outlook Report
Water Supply Pro - Doc Type
Publication
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<br />ARKANSAS RIVER BASIN <br />as of March 1, 1999 <br /> <br />Mountain Snowpack' (inches) <br /> <br />Precipitation' (% of average) <br /> <br />~Current ...-.-Average <br />__Maximum __Minimum <br /> <br />I_Monthly OIVear-to.date I <br /> <br /> 20 <br /> 18 <br /> 16 <br />.5 14 <br />.; <br />c: 12 <br />D <br />ii <br />> 10 <br />'5 <br />t7' <br />w <br />.. 6 <br />D <br />- <br />to <br />:: 6 <br /> 4 <br /> 2 <br /> 0 <br /> Jan Feb Mar Apr May <br /> <br /> <br /> 180 <br /> 160 <br /> 140 <br />D <br />Q 120 <br />I! <br />D <br />~ 100 <br />... <br />0 <br />1: 80 <br />D <br />l:! <br />D 60 <br />a.. <br /> 40 <br /> 20 <br /> 0 <br /> Oct Nov Dee Jen Feb Mar Apr May <br /> <br /> <br />.Based 00 selected statiODS <br /> <br />The snowpack in the Arkansas Basin has gone from 86% of average on February 1 to 79% of <br />average on March 1, The snowpack is extremely variable from north to south, with amounts at <br />90% of average in the Arkansas Basin above Salida, and only 55% of average in the Purgatoire <br />Watershed, There is 80% of the amount of snow there was last year at this time. Precipitation <br />during February was only 77% of average for the month, and the wateryear total is now 115% of <br />average, Combined reservoir storage levels in the Basin are at 211 % of average for this time of <br />year, which is 92% of the amount last year at this time, All of the streamflow forecasts for this <br />runoff season are below average, The forecasts are variable throughout the basin depending mostly <br />on location and current snowpack conditions, They range from only 62% of average on the <br />Cucharas River near Laveta, to 95% of average on the Arkansas River at Salida, <br />
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