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<br />~ ' <br /> <br />complex mountainous terrain is a major area of <br />uncertainty for winter orographic weather modifica- <br />tion. The ~asic approach will be to monitor AgI <br />plumes from ground generators, or AgI lines <br />released from aircraft, with an airborne ice <br />nucl eus counter simi 1 ar to the work reported by <br />Super (1974). Ground generators will be manually <br />operated at one or more of the sites shown on <br />Figure 1. Generators will be transported to the <br />sites by helicopter or snowmobile depending upon <br />location. <br /> <br />Ground-released AgI plumes will be sampled by <br />aircraft under VFR (visual flight rule) conditions <br />by making horizontal passes, generally from 100 to <br />1000 ft (30 to 300m) above the ground, approxima- <br />tely perpendicular to the wind at a given downwind <br />distance. Normally at least two passes will be <br />made at each altitude so that the lag time of the <br />counter can be used to estimate the plume edge on <br />each side. Pairs of passes will be made at alti- <br />tude increments from near the surface to above the <br />plume, providing a vertical and horizontal cross- <br />section through the plume. The fine structure of <br />the plume is not available with this approach due <br />to the slow counter response as ice crystals must <br /> <br />6 <br />