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Correspondences Related to CREST and Funding of CREST Program
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Correspondences Related to CREST and Funding of CREST Program
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Water Supply Protection
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Correspondences Related to CREST and Funding of CREST Program
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Correspondences Related to CREST and Funding of CREST Program
Water Supply Pro - Doc Type
Correspondence
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the other objectives. Production of <br />of increased snowpack, if any, will <br />water and confirmation of the <br />be thoroughly studied as the <br />resulting increases will help in <br />demonstration progresses. Suspension <br />deciding on the best use and <br />criteria will be used and revised <br />distribution of the additional water. <br />during all phases of the program as a <br />supplies. ,,.. <br />safeguard against potential flooding, <br />percent of the available moisture in - <br />avalanche or other hazards. <br />Environmental and social impacts, as. <br />surface as snow. <br />well as the reduction of any -risks <br />Public Involvement and understanding <br />associated with cloud seeding, will <br />of the CREST program and its <br />be considered throughout the <br />objectives are vital to the success <br />demonstration. These factors will <br />of the demonstration. Public <br />influence the use of the technology, <br />acceptance and support are important <br />and will.help in the evaluation of <br />to the realization of a fully <br />the results and benefits of the CREST <br />..operational weather modification <br />program. . The enxi ronmental effects <br />program in the Colorado River Basin. <br />percent, or another 1 percent-of the- -,-- <br />causes ice crystals to farm because <br />The principles involved in seeding <br />winter (orographic) clouds are <br />relatively simple. The flow of moi s <br />air over mountain barriers produces <br />liquid water droplets through <br />condensation as the air is forced <br />into colder temperatures at higher <br />elevations. These droplets tend to <br />remain in the liquid state without <br />freezing at temperatures lower than <br />0oC (32 °F) because of the purity of <br />the water and the absence of foreign <br />particles in the free atmosphere; <br />they are referred to as "supercooled <br />droplets" and the clouds they form <br />and silver iodide, which has a <br />physical-structure similar to that of <br />natural Ice crystals. ice crystals <br />t formed by seeding can convert more <br />supercooled water to snow, and <br />thereby increase the "efficiency" of <br />the clouds. <br />The technology of modifying winter <br />cloud systems to increase mountain <br />snowpack has been developing over the <br />past 30 years. Evidence about the <br />potential for snowpack augmentation <br />in the high mountains of the Colordo <br />River Basin is largely based on <br />statistical data from past projects <br />y �_ <br />SEEDING. WINTER STORMS t. _ . �. ; <br />JF are called supercooled clouds. If <br />ice particles occur naturally, or are <br />In the high country of- "the Colorado,. <br />introduced artifically into these <br />River Basin, as in all other winter <br />supercooled clouds, the ice particles <br />storm areas, only an estimated 10 <br />will grow at the expense of the <br />percent of the available moisture in - <br />droplets, and begin to reach the <br />seasonal-storms falls to the surface <br />surface as snow. <br />as snow. The remaining moisture. - <br />stays in the atmosphere and disperses <br />,If the concentration of natural ice <br />without ever changing to snow or <br />..., particles is too low for <br />rain. Cloud seeding can improve the <br />precipitation to form and fallout to <br />efficiency of the natural - :; _:. <br />:s : occur, the ice particle concentration <br />precipitation process. and, under. <br />_. can be i ncreased through the use of <br />favorable conditions, increase <br />seedi ng material . The - most common <br />seasonal precipitation by 10 to 15 <br />seeding agents -are dry ice, which <br />percent, or another 1 percent-of the- -,-- <br />causes ice crystals to farm because <br />available moisture. <br />of its extremely cold temperature, <br />The principles involved in seeding <br />winter (orographic) clouds are <br />relatively simple. The flow of moi s <br />air over mountain barriers produces <br />liquid water droplets through <br />condensation as the air is forced <br />into colder temperatures at higher <br />elevations. These droplets tend to <br />remain in the liquid state without <br />freezing at temperatures lower than <br />0oC (32 °F) because of the purity of <br />the water and the absence of foreign <br />particles in the free atmosphere; <br />they are referred to as "supercooled <br />droplets" and the clouds they form <br />and silver iodide, which has a <br />physical-structure similar to that of <br />natural Ice crystals. ice crystals <br />t formed by seeding can convert more <br />supercooled water to snow, and <br />thereby increase the "efficiency" of <br />the clouds. <br />The technology of modifying winter <br />cloud systems to increase mountain <br />snowpack has been developing over the <br />past 30 years. Evidence about the <br />potential for snowpack augmentation <br />in the high mountains of the Colordo <br />River Basin is largely based on <br />statistical data from past projects <br />y �_ <br />
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