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<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 />3. Obsenations within the Seeding Plumes <br />Prior to the start of seeding on 26 January the mobile radiometer ascended the plateau, <br />tra\'eling from HQ to RRS (Fig. 1) between 0910 and 1020. Data from this traverse are shO\..n in Fig. <br />41. During this period most of the liquid water was observed over the Sanpete Valley and the lower <br />foothills of the plateau. Along the edge of the top of the Plateau and at RRS very little liquid water <br />was observed. Between 1045 and 1245 six passes were made with the mobile radiometer between <br />RRS and the Junction of Highways 31 and 264 (Fig. 1). The temperature at the surface ranged from <br />-6'" to -8". Liquid water depths rarely exceeded 0.04 mm on these passes, and only occasional light <br />sno\\fall was noted. This is consistent with the very weak radar echo (Figs. 38-40) over the plateau <br />prior to 1100. <br />Beginning at about 1250, and continuing through 1600, the mobile radiometer made ten <br />passes in tandem with the Ctah instrumented van (called Starship) bet\veen RRS and Jet. 311264. <br />The Starship monitored SF", ice nuclei and re{;{)rded 2D-C images along the route. Figure 42 shows <br />data from the first two passes between 1250 and 1328. Radar returns over the highway were <br />increasing during this time, and light to moderate sno\\:fall was observed. On both passes SF 6 and <br />ice nuclei plumes were encountered at about the same location (1.5-3.0 Ian northwest of RRS) <br />\vithin a region of slightly enhanced liquid water. On the first pass the SF 6 plume was coincident <br />with a small scale liquid maximum, while the second plume interception matched a liquid water <br />minimum, so it is not clear from these two passes if seeding was depleting the cloud liquid. The <br />temperatures at the surface were near the threshold of activation for the AgI solution in use. <br />Also between 1314 and 1317 the research aircraft, flying at about 3250 m on its west track, <br />encountered SF(jand ice nuclei plumes. The locations of the Starship and aircraft plumes are shown <br />in plan view in Fig. 43. With the southwest to west-southwest flow detected at HAS and RRS, it is <br />apparent that the Starship plume originated from the HA.S generator. The aircraft, however. was <br />apparently detecting mainly the AHS generator plume, although some SF 6 values slightly above <br />detectable background were noted 4-9 kIn north ofRRS, and these might have been the plume from <br />HAS. Although the aircraft flew its east and we~t tracks numerous times between 1124 and 1400, <br />the plume encountered shortly after 1300 was the most definitive and accounted for nearly all of the <br />SFfdetected on this flight. On its t\\l0 stops at RRS bet\\leen 1248 and 1328 the van detected no SF6 <br /> <br />54 <br />