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<br />I ~ 'i <br />:1 <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 />I <br />I <br />I <br />I <br /> <br />Introduction <br /> <br />The Rocky Mountains, garbed in their majestic snows for most of the year, store <br />water for half a continent. To scientists seeking ways to augment water supplies <br />in the western United States by enhancing natural precipitation, they and the <br />atmosphere above them represent a vast natural resource. Their allure is only <br />increased by the fact that they arEl relatively sparsely populated. <br /> <br />Motivating federal government scientists to augment water flowing in the Colorado <br />River Basin is the fact that the United States, owing to the Colorado River <br />Compact, must send to Mexico. 1.5 million acre-feet of high~qualitywater each <br />year. I Frequently the United States cannot meet its Compact obligations while <br />preserving the water rights of 'users in the mountainous Upper and populous Lower <br />Basin States" It is no wonder that scientists looked to the Upper Basin States <br />for sites to conduct orographic cloud seeding experiments. <br /> <br />In addition to these political realities, climatology and other considerations make <br />the San Juan Mountains of Southwestern Colorado prime candidates for cloud seed- <br />ing experimentation. First, the Colorado River Basin Pilot Project (CRBPP or Pilot <br />Project) was conducted in the area;2 next, operational snowpack augmentation went <br />on for a decade; and finally, th,e U.S. Bureau of Reclamation has proposed the area <br />for a future federal cloud seeding demonstration project called the Colorado River <br />Enhanced Snowpack Test (CREST).3,4 Therefore, federal scientific interest in <br />. pursuing weather modification potential in Colorado's San Juan Mountains is likely <br />to continue in the decades ahead. <br /> <br />While studies have focused not only on the effects of cloud seeding on snowpack <br />and runoff, but also on such impacts as effects of increased snow on flora and <br />fauna, avalanche occurrence, andl highway snow reinoval costs, very little' is known <br />about community response to sIlowpack augmentation in the San Juan area. One <br />early study was' a technology assessment of winter orographic snowpack augmenta- <br />tion (WOSA).S This technology assessment reviewed the. economic, social, and <br />environmental impacts of WOSA a.Ild concluded . <br /> <br />The environmental, economic, and social impacts of WOSA on the high <br />mountain areas . . .. are, almost uniformly negative, but are of only <br />moderate intensity. <br /> <br />There is no need for the additional water provided by the WOSA system <br />in the high mountain are:ilS that would bear these negative impacts for' <br />the benefit of other areas . . . . There appear to be sufficient <br />benefits from the WOSA water increment . that the drawbacks to. the <br />target area residents could be offset by a program of alleviation and <br />compensations, providing that the necessary institutional arrangements <br />can be made.6 <br /> <br />*Upper Basin states include Colo~rado, Wyoming, Utah and New Mexico. Lower <br />Basin states are Arizona, Cillifornia, and Nevada. <br /> <br />I <br />