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<br />PREFACE <br /> <br />The Steamboat Springs area, on the windward <br />side of the Park Range of the Rocky Mountains in <br />Colorado, is almost ideal for physical experimenta- <br />tion on orographically induced convective clouds. <br />The valleys and slopes of the Range are reasonably <br />accessible for instrumentation and observation; the <br />isolated mountains west of Steamboat Springs pro- <br />vide excellent vantage points for radar surveillance <br />and for high-altitude nucleation. A large part of <br />the target area is over Government-owned land, <br />and drainage from the area is into the Bureau of <br />Reclamation's Colorado River Storage system. <br />The experimental site was recommended to the <br />Bureau of Reclamation by independent meteoro- <br />logical consultants, including Bollay Associates, <br />Inc., of Boulder, Colo., an organization having con- <br />siderable previous experience in research on <br />weather modification. This firm performed the <br />investigations described in this report under con- <br />tract with the Bureau of Reclamation. The investi- <br />gations, designated as Phase I of the Park Range <br />program, were started in November 1964 and com- <br />pleted in June 1965. Phase II of the program is in <br />progress and will be the subject of a subsequent <br />report. <br />The Park Range program is intended to deter- <br />mi,ne to what extent the precipitation in a moun- <br />tainous region can be increased by artificial nuclea- <br />tion of moisture-bearing cloud formations. Phase I <br />was devoted to the collection and processing of <br />nuclei and to the study of diffusion and precipita- <br />tion processes under natural conditions. The "set- <br />up" of facilities and equipment, the methods of <br />tracking storms over the target area, the measure- <br />ments and observations, and the results and con- <br />clusions of Phase I are embodied in this report. <br />Phase II involves controlled artificial nucleation of <br />moisture-bearing clouds over the same target area <br /> <br />with an evaluation of effect by comparison of pre- <br />cipitation and runoff under artificially induced and <br />under natural conditions. <br />This report on the Phase I part of the program <br />describes the experimental plan, the facilities, and <br />equipment used in the studies; the methods of <br />determining nuclei concentration; and the diffusion <br />and precipitation processes in the Park Range area. <br />Phase I data are analyzed for their application to <br />the Phase II program. Also include~ are support- <br />ing maps, photographs, climatological and meteoro- <br />logical data, graphs, and charts. <br />Briefly, the Phase I study shows that conventional <br />artificial nuclei generators can be effectively used <br />from a selected site for a majority of spring and <br />winter storms in the area. The concentration and <br />extent of targeting with artificial nucleation can be <br />determined for a particular storm by testing snow <br />samples for silver concentration throughout the <br />target areas. This concentration and extent can be <br />checked with zinc sulphide, which was used in the <br />Phase I operation as the tracer material for the <br />diffusion tests. The ratio of natural to artificially <br />formed snow crystals can be reasonably expected to <br />indicate the extent of participation by the artificial <br />freezing nuclei. <br />The continued pursuit of the Park Range studies, <br />together with those of other cooperating firms and <br />agencies, can contribute considerably to the learn- <br />ing which is necessary if man is to tap the vast re- <br />source of atmospheric water. <br />The extensive systems of storage reservoirs and <br />irrigation facilities constructed by the Bureau of <br />Reclamation over the past 64 years have been most <br />effective in their purpose of reclaiming the semiarid <br />land in the 17 western States to useful production. <br />These reservoirs serve to regulate the flow of rivers, <br />which would otherwise be lost, by storing excess <br /> <br />III <br />