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<br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />t <br />. <br />. <br />t <br />t <br />. <br />. <br />t <br />t <br />. <br />. <br />. <br />t <br />t <br />. <br />t <br />t <br />t <br />. <br />. <br />t <br />t <br />. <br />t <br />. <br />. <br />. <br />t <br /> <br />A significant amount of aircraft plume tracing near mountains has been done on earlier projects. <br />Super (1974) discussed VFR plume tracing using an ice nucleus counter over the Bridger Range <br />of Montana. The findings of successful transport and dispersion of the seeding agent provided <br />physical support to the strong statistical suggestions that seeding resulted in seasonal snowfall <br />increases of 15 percent or more over the intended target area (Super and Heimbach 1983). Later <br />IMe sampling with an aircraft instrumented to measure cloud microphysics showed AgI over the <br />target, and also associated seeded ice crystal plumes when SL W clouds were cold enough for the <br />AgI to be effective (Super and Heimbach 1988). <br /> <br />When synoptic conditions are deemed appropriate by the project forecaster, a serial rawinsonde <br />release will be made upwind of the target area, and the sounding data used to initialize the WMI <br />Targeting Model. This targeting model has its roots in the Guide Model developed by Rauber et <br />at. (1988), but has been updated and modified to run in real-time on a Pentium-class Pc. The <br />output from the targeting model will be used to predict the transport and dispersion of the <br />seeding agent, and the aircraft sampling.flight path will be planned accordingly. Examples of the <br />output from the model from a simulation of ground based seeding in British Columbia are <br />provided in Figure 11 (plumes from ground-based sites) and Figure 12 (sample terrain). <br /> <br />Weather Damage Modification Program 27 <br />