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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 />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />1 <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />An earlier estimate on March 20,2003 of the seeding effects for the San Juan Water Conservancy District's seeded <br />area using just the historical and current observations for the two Snotel sites on Wolf Creek Pass indicated an <br />additional 1.8S" of precipitation on the Southwest side of Wolf Creek Pass. This amount of extra water over the <br />Upper San Juan watershed would produce a potential additional 29,000 Ac.Ft of runoff for the San Juan River <br />through Pagosa Springs. <br /> <br />An analysis of the timing of the precipitation increases from the seeding efforts indicated that slightly more that <br />half (53%) of the precipitation increase over the Upper Animas and La Plata River Basins occurred during the <br />February through April 7, 2003 operational period. This same relationship was true for the Eastern San Jaun <br />Program Area (54%) even though the Program ended three weeks earlier than the Animas Basin Program. This <br />was primarily due to the nature of this winter's weather systems in that thefust three months of the Seeding <br />Program weather was in a drying trend and the last two months plus of the Program's weather was all near normal. <br /> <br />The procedure for estimating the seeding increases was bases on two research analysis conducted by Western <br />Weather Consultants, LLC of two separate seeding programs ** conducted over the Colorado mountains utilizing <br />similar seeding applications and weather event identification criteria. Both of these analyses produced extremely <br />similar evaluations of seeding responses to the systems being treated. A composite of these results utilizing a <br />conservative estimate of these seeding responses to the associated prevailing wind direction of the storm system <br />has been developed by Western Weather Consultants and forms the basis of this process to estimate seeding <br />increases. <br /> <br />Western Weather Consultants also followed the accumulation of the precipitation at the various Snotel Sites in the <br />Colorado Mountain Region throughout this winter's seeding season. We looked at how the precipitation was <br />accumulating as a percentage of what normally accumulates during the seeding season. Plots of the analysis of this <br />data are included for the periods ending February 1,2003, March 1, 20()3 and AprilS, 2003 to show the trend of <br />the winter's precipitation accumulation and the impact of the large storm of mid-March, 2003 <br /> <br />** Precipitation increase estimates were made utilizing previous research results from the Colorado River Basin <br />Pilot Project (research randomized seeding program), June, 1976; and 10 and 16 Year Data Sets from two separate <br />precipitation sources for the VaillBeaver Creek Seeding Program (operational seeding program), March, 2001 <br /> <br />3 <br />
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