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Last modified
7/28/2009 2:32:19 PM
Creation date
4/11/2008 3:38:39 PM
Metadata
Fields
Template:
Weather Modification
Contract/Permit #
85-5071
Title
Cooperative Weather Modification Research Program - 1985 Field Operations Plan
Date
1/1/1985
State
UT
Weather Modification - Doc Type
Report
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<br />. <br /> <br />. <br /> <br />1. Introduction <br /> <br />Winter orographic clouds have been identified for some time (Grant <br />and Kahan, 1974) as likely candidates for snowfall augmentation through <br />cloud seeding. The State of Utah operational snowfall augmentation pro- <br />ject presents an opportunity for gatheroing research information for <br />improving future such seeding projects. In response to this opportunity <br />and in agreement with recommendations of the Weather Modification <br />Advisory Board (1978), the Nationall Oceanic and Atmospheric <br />Administration (NOAA) initiated a cooperative program of weather modifi- <br />cation research involving itself, the State of Utah, and local govern- <br />mental bodies. <br />Research under this cooperative program has been conducted in the <br /> <br /> <br />Tushar Mtns area near Beaver, Utah in rec:ent years as an adjunct to the <br /> <br /> <br />State of Utah operational project. An initial field effort was con- <br /> <br /> <br />ducted by the Utah State University WatE~r Research Laboratory during <br /> <br />February and March, 1981. Results of that preliminary research (Hill, <br /> <br /> <br />1982) were that significant amounts of supercooled liquid water were <br /> <br /> <br />present in the clouds and that most trcljectories of precipitation par- <br /> <br /> <br />ticles forming from this water would intersect the mountain. <br /> <br />A second field effort was conducted by the Utah Department of <br /> <br />Natural Resources Division of Water Resources (UDWR) from 15 January to <br /> <br />15 March, 1983. UDWR was prime contractor and other groups with <br /> <br />appropriate expertise provided scientific and technical assistance <br /> <br />through sub-contracts (Griffith et~. (19:83), Henderson (1983), Rauber <br /> <br /> <br />and Grant (1983), Sassen (1983) and Stone (1983)). Results of that <br /> <br />research (Long, 1984) were that the amount of liquid water in the clouds <br /> <br />increases from a position 5-10 km west of the western base of the <br /> <br />. <br /> <br />. <br /> <br />.' <br /> <br />. <br /> <br />.. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />1 <br /> <br />. <br />
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