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Last modified
7/28/2009 2:34:37 PM
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4/11/2008 4:23:06 PM
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Weather Modification
Title
Scientific Weather Modification Experimentation in the United States
Date
8/25/1984
Weather Modification - Doc Type
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<br />~ <br /> <br />Presented at the Ninth International Cloud Physics Conference <br />Tallinn, U.S.S.R. <br />August 25, 1984 <br /> <br />SCIENTIFIC WEATHER MODIFICATION <br />EXPERIMENTATION IN THE UNITED STATES <br /> <br />Bernard A. Silverman <br />Bureau of Reclamation <br />Denver, Colorado U.S.A. <br /> <br />1. Introduction <br /> <br />This paper discusses recent scientific weather modification research in the <br />United States. Four large precipitation enhancement research programs are <br />briefly reviewed: the recently completed HIPLEX-l (Montana High Plains <br />Experiment) and FACE-2 (confirmatory Florida Area Cumulus Experiment) experi- <br />ments, the ongoing SCPP (Sierra Cooperative Pilot Project) program and the <br />planned CREST (Colorado River Enhanced Snowpack Test) demonstration program. In <br />addition, highlights of selected activities in three areas of related research <br />are presented: 1) dual-channel microwave radiometer applications, 2) laboratory <br />studies of the ice nucleating properties of silver iodide complexes, and 3) eva- <br />luation of experiments by monitoring the expected chain of physical events <br />following seeding. Finally, the probable nature of future scientific weather <br />modification experimentation in the United States is discussed. <br /> <br />2. HIPLEX-l <br /> <br />HIPLEX was aimed at establishing the physical basis for enhancing beneficial <br />growing season precipitation from convective clouds on the High Plains of the <br />United States. HIPLEX-1 (Bureau of Reclamation, 1979) was a randomized, double- <br />blind exploratory experiment to test the static mode seeding concept for summer <br />convective clouds over the Montana High Plains. The experimental unit of <br />HIPLEX-1 was semi-isolated cumulus congestus clouds which develop precipitation <br />naturally through the Bergeron mechanism, that is ice crystal growth by vapor <br />diffusion followed by riming into graupel. Many of these clouds do not rain to <br />the ground at all. The objective of the static seeding was to provide an opti- <br />mum concentration of ice particles for the available liquid water, about 10 per <br />liter, and initiate the precipitation process earlier and lower in altitude in <br />the developing clouds than would occur naturally. It was hypothesized that the <br />efficiency of the natural precipitation process would be improved by the seeding <br />and thereby lead to both additional precipitation and to an increase in the pro- <br />portion of clouds that precipitate. <br /> <br />Detailed criteria and procedures for selecting and classifying test cases, for <br />performing the seeding and for the collection of observations to be used in <br />calculating response variables were prescribed. Based on preliminary explora- <br /> <br />1 <br /> <br />I. <br />
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