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Last modified
7/28/2009 2:34:36 PM
Creation date
3/5/2008 2:26:26 PM
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Template:
Weather Modification
Title
Physical Structure of Northern Colorado River Basin Cloud Systems
Date
9/1/1985
State
CO
Weather Modification - Doc Type
Report
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<br />14 <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 />1 <br />I <br />I <br />I <br />I <br /> <br />Additional work emphasizing the transport and dispersion of silver <br />iodide in the Climax region was conducted by Reid (1976) and Orgill <br />(1971). Re~d studied the dispersion of silver iodide with aircraft and <br />surface measurements. Orgill (1971) simulated the transport of seeding <br />material using a physical model of the Climax region in a wind tunnel. <br />(2) Park RanRe AtmosDheric Water Resources Proaram (PRP) <br />The PRP was the first major wintertime weather modification field <br />effort to conduct an extensive physical evaluation of the effects of <br />cloud seeding to augment precipitation (Rhea et al., 1969). Analysis of <br />the physical data was supported by the use of a steady-state numerical <br />model of orographic precipitation developed at EGG Inc. (Willis, 1970). <br />A significant number of transport and dispersion studies were also <br />conducted. The majority of the physical results of the experiment were <br />based on data collected during the 1968-69 field season. The analysis <br />of the 1968-69 data set incorporated both the case study approach as <br />well as statistical analyses of the precipitation data. Unfortunately, <br />only limited data were presented concerning natural cloud system <br />structure. The majori ty of the data were associated with identification <br />of seeding signatures. This was primarily through analysis of ice <br />crystal replicas, measurements of ice nuclei and silver in snow during <br />pulsed seeding events. <br />The major results of the PRP based on five winter seasons ,of <br />operation are summarized by Rhea et ale (1969). During the program, <br />significant amounts of seeding material were found in target area <br />precipitation, in timing and location with calculated occurrence of <br />seeding effects. In several case studies, a positive seeding effect was <br />clearly evident, During the seeding period, small hexagonal plates were <br />
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