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CWCB Wintertime Weather Mod Report
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CWCB Wintertime Weather Mod Report
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Last modified
7/30/2009 12:11:35 AM
Creation date
9/30/2006 9:03:59 PM
Metadata
Fields
Template:
Water Conservation
Project Type
General OWC
Applicant
Weather Modificaton
Project Name
Colorado Weather Modification Program
Title
CWCB Wintertime Weather Modification Report Fall 2002 - Spring 2003
Date
7/1/2003
Water Conservation - Doc Type
Final Report
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<br />4 <br /> <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 />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />occur during a variety of weather patterns, which tend to vary in a somewhat predictable <br />manner according to the time of year. During the winter period (December-February), <br />many of these precipitation events resulted from strong zonal (west-east) flow, with mid- <br />and high-level Pacific moisture moving over Colorado. Satellite images during these <br />zonal events were often very impressive, with high cloud cover (very bright on the IR <br />imagery) covering large portions of the western U.S. Deep upper-level trough situations <br />were also responsible for some of the precipitation events. Storm systems traversing the <br />southwestern United States and southern Rockies favored the spring and fall seasons. <br />, Typically the more significant precipitation amounts occurred in southwesterly flow <br />ahead of the surface frontal system (sometimes well in advance), although some did <br />occur in northwesterly flow following frontal passages. A thick shield of high-level <br />cloud cover was evident in most of these significant precipitation events, suggesting a <br />large amount of high-level moisture. Strong upper-level winds and a jet core near <br />Colorado were very often associated with these precipitation events. <br /> <br />2.3 Frequency of Significant Storm Events <br /> <br />An analysis was conducted using daily precipitation records from four Natural <br />Resources Conservation Service SNOTEL sites in the 9600 - 10600 foot elevation raJ?ge <br />in the mountains northwest and northeast of Gunnison, Colorado. The four sites were <br />Brumley, Butte, Independence Pass, and Park Cone. Days with approximately 0.4" or <br />more of precipitation during the October-April season during the 'years from 1990 <br />through 2001 were identified. It was found that 12 or 13, O.4-inch or greater storm days <br />occur during the October-April season on average. April had the highest frequency of <br />these events (2.7 per season), followed by November and February (2.1 per season). <br />December had the lowest frequency with approximately Istorm day per season. An <br />average amount of one inch or greater occurred at these SNOTEL sites on only about <br />10% of these storm days. <br />
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