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WSP08695
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Last modified
7/29/2009 9:54:02 PM
Creation date
10/12/2006 3:10:15 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8027
Description
Section D General Correspondence-Federal Agencies
State
CO
Date
1/1/1967
Author
Archie M Kahan
Title
US Department of Interior-United States Geological Survey Water Resources Division and Quality of Water Branch-1967-1968-Irrigation Operators Workshop 1967-Atmospheric Water Resources-1967
Water Supply Pro - Doc Type
Report/Study
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<br />\\.~~ <br /> <br />. <br /> <br />. <br /> <br />develop end test new techniques and procedures. Before arry <br />field program is tmdertaken, certain supporting studies are <br />desirable. One of the most important of these is the clima- <br />tology of the area. This is incoI1>Orated into all of our <br />present end planned field experiments. <br /> <br />Field research is being conducted in the Colorado River Basin <br />by two private organizations, with support fran two Federal <br />agencies for specialized measurements. E. Bollay Associates <br />is working in the Park Range area of the Colorado Rockies <br />developing a new evaluation technique, power spectrum analysis, <br />and also procedures for detecting seedable storm systems and <br />methods for determining the lateral and vertical extent of <br />the seeded area. This group uses ground-based silver iodide <br />generators. <br /> <br />Meteorology Research, Inc. is studying the behavior of oro- <br />graphically induced convective clouds near Flagstaff, Arizona. <br />One of the goals here is the detennination of quantitative <br />requirements for seeding convective clouds. They are also <br />studying buoyancy effects. When a drop of water freezes or <br />when water vapor condenses, heat is released. The heat warms <br />the surrounding air and makes it a little lighter. This air <br />tends to rise, and the rising motion is the buoyancy effect. <br />It is induced artifically when seeding material initiates <br />the freezing process. <br /> <br />Three university groups, South Dakota School of Mines and <br />Technology, University of Wyaoing, and Montana State University, <br />are conducting field studies in the Missouri River Basin. The <br />University of Wyoming is studying cap cloud precipitation, <br />which has already been discussed briefly. There can be no <br />question about the effect of seeding these cap clouds. Pre- <br />cipitation rarely falls naturally fran them, but when they are <br />seeded (Wyaoing uses a ground-basedsilver iodide generator) <br />snow falls; when the generator is turned off, the snow stops; <br />when the generator is moved, the area of snowfall moves. <br />There are indications that one silver iodide generator could <br />provide perhaps 450 acre feet of water in the form of additional <br />high""1llOuotain snowpack per day of cap cloud occurrence. About <br />1,000 of such generator-day units of operation ahould be avail- <br />able during most winters on the several mountain ranges of <br />WYOllling . <br /> <br />Montana State University is studying the downwind effects of <br />artificial nucleation in en orographic storm situation. Some <br />scientiats have suggested that seeding one area results in <br />changes in the precipitation downwind, even though no seeding <br />material is involved. Montana States' team of researchers <br /> <br />12 <br />
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