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<br />II <br /> <br />was exposed for timed intervals during snO\-1fall periods furnishing some <br /> <br />valuable information on precise snowfall rates. <br /> <br />C. W.S.S.I. Data <br />1. SnO\o1fall <br /> <br />l~estern Science Services, Inc. (W.S.S.I.) operated ~30 precipitation gauges <br /> <br />over the San Juans as part of the San Juan Project. These data were always <br /> <br />made available for each storm studied as soon as they were available. The <br /> <br />data are discussed in Hartzell et al. (1975) and Hartzell and Crow (1976). <br /> <br />They \o1ere plotted and analyzed as part of the synthesis of each storm. The <br /> <br />important characteristics of the snowfall are summarized in each case study. <br /> <br />2. Ice .Nuclei <br /> <br />W.S.S.I. also operated Bigg-Warner ice nucleus counters at Pagosa Pines <br /> <br />and Piedra (both near Pagosa), and at Wolf Creek Pass. These data were <br /> <br />examined carefully for each seeded storm studied and several plots of the <br /> <br />data are presented in the case studies. <br /> <br />D. E.G. & G. Data <br />E.G. & G. conducted the seeding operation for the San Juan Project. The <br /> <br />seeding logs ,vere provided for each seeded storm studied. As part of their <br /> <br />operation they released rawinsondes from the Durango airport at three-hourly <br /> <br />intervals during all randomized case studies. In addition, they made three- <br /> <br />hourly soundings on storms flown by the research aircraft if the storm was <br /> <br />not one of the randomized c.ase studies. <br /> <br />The other set of data collected by E.G. & G. which proved especially <br /> <br />valuable in understanding the storm structure and its evolution with time <br /> <br />\.;ras surface winds. E.G. & G. had 10 to 12 'vind stations located between, <br /> <br />Wolf Creek Pass and Farmington. These data were telemetered in real time <br /> <br />at three hourly intervals to the E.G. & G. forecast office in Duiango. <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />II <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />