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<br />- g - <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 />I <br />I <br />I <br />I <br />I <br /> <br />Therefore, our primary te st for precipitation augmentation is between the in- <br />put and output of the experiment without asking in detail what the transfer <br />function is in between. <br /> <br />Besides these measurements, we desire knowledge of the more con- <br /> <br /> <br />ventional rneteorological parameters. These include surface winds and tem- <br /> <br /> <br />perature, vertical wind and temperature profiles, radar pictures of storms, <br /> <br /> <br />and snowcourse and stream gauge measurements for long term averages and <br /> <br /> <br />loss calculations. <br /> <br />The experimental area is centered on Stearnboat Springs, Colorado. <br />It has a relatively high annual precipitation, a mountain ridge--the Fark <br />Range -- to provide orographic effects, is relatively accessible and is an <br />important source of water--via the Yampa and Green Rivers- -to the Colo- <br />rado River. During the winter months, precipitation on the Park Range is <br />snow. The climatology of the valley is shown in Table I; climatological sta- <br />tion locations are shown in Figure 5. Storm trajectories are confined large- <br />ly to the NW - SW quadrant. <br /> <br />Our measurement network IS shown in Figure 6; it consists of 15 <br /> <br /> <br />snow-rate stations, 5 meteorological stations, 1 diffusion test and artificial <br /> <br /> <br />nuclei generation station, 22 snowcourses, 1 radar and rawinsonde station, <br /> <br /> <br />1 nuclei count station, and 3 stream-gauging stations. <br /> <br />For diffusion and artificial nuclei generating work, we selected the <br /> <br /> <br />Emerald Mountain site because of its height (8300 feet), accessibility, and <br /> <br /> <br />alignment with the target area. Optical-type snow- rate sensor s are used <br /> <br /> <br />throughout the network for measurement of the prime variable; these sensors <br /> <br /> <br />are routinely serviced on an 8;.;day schedule and after every storm. The pre- <br /> <br /> <br />cipitation- rate records are recorded on conventional analog recorder s, man- <br /> <br /> <br />ually reduced and computer processed. Appendix C presents the program <br /> <br /> <br />Ii sting. <br /> <br />We have built our field operation around a small group of technical <br />personnel and hire locally whenever additional labor is required. The overall <br />