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<br />to rather than toward the Tushar Mtns. If material does follow a trajec- <br /> <br />tory into clouds over the Tushar Mtns then delivery is limited by the <br /> <br />narrow plume. Even with a narrow plume only 36% of the soundings con- <br /> <br />sidered showed seeding material was delivered to the clouds. In one case <br /> <br />seeding material was delivered to the clouds only from a high-altitude <br /> <br />generator above the "dead" air. <br /> <br />Che~ical analysis of the snowpack showed little silver above back- <br /> <br />ground levels, and indium concentrations above background were less than <br /> <br />~.>\--"'''''''''''-'''''''1 <br /> <br />expected naturally. <br /> <br />These results probably were due in part to the <br /> <br />limited delivery of seeding material likely accomplished in 1983. <br /> <br />Additional factors restricting the number of samples with silver or indium <br /> <br />concentrations above back ground were the compaction of the snowpack and <br /> <br />the 4 cm resolution of the snow sampling technique. <br /> <br />f. <br /> <br />Climatological representativeness of 1983 weather. <br /> <br />Weather <br /> <br />during the 1983 research period was abnormal in several respects. Zonal <br /> <br />rather than meridional flow was dominant. At 700 mb and 500 mb winds were <br /> <br />more southerly than normal and temperatures were warmer than normal. <br /> <br />Rawinsonde-derived cloud tops were lower and warmer than usual, and STORM <br /> <br />duration was shorter than usual. At Beaver minimum surface temperatures <br /> <br />were above normal and precipitation was above average. <br /> <br /> <br />-- -......--.- <br /> <br />------ <br />1983 field investigations and physical <br /> <br />Principal conclusions of the <br /> <br />analysis are that substantial amounts of supercooled liquid water are pre- <br /> <br />sent in the study clouds, primarily in their lower levels and over the <br /> <br />Tushar. Mtns, but that delivery of seeding material to the clouds from low- <br /> <br />altitude ground generators is frequently limited by meteorologica~ .c:...o~~/ <br /> <br />._~,..,.. -.;.-,.-,--;:.,.,.--,...~-...,.-.-- <br /> <br />ditions. <br /> <br />....--. .:::>:"'" <br /> <br />xxvi <br /> <br />