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<br />2.4 <br /> <br />in the 1983-84 winter season. It was selected primarily to avoid contami- <br />nation of the snow samples with materials blown from HALO's maintenance <br />yard salt/sand piles. Tests were to be made to determine whether or not <br />there was a contamination problem. On one or two occasions during this <br />field season, two simultaneous sets of samples were collected. One set <br />was collected at HALO adjacent to the Ka-band radar while the other was <br />collected approximately 1 kIn to the east. Chemical comparisons of the <br />contents of the samples were then made to determine the magnitude if any <br />of contamination. <br /> <br />So that it was possible to track silver iodide from a particular <br />aerosol generator over the observing sites, two ground-based generators <br />were prepared for use at Cisco Butte directly upwind of the Kingva1e site. <br />In addition to the AgI unit already at Cisco, a mobile generator was also <br />taken to the site. This unit was to be used for releasing non-ice <br />nucleating indium sesquioxide aerosols simultaneously with or separately <br />from the AgIo <br /> <br />Between 1 January and 31 March 1985, all field activities related to <br />this task were completed for this 1984-85 winter season. The main effort <br />included the collection of one hundred ninety (190) freshly-fallen sequen- <br />tial snow samples at the Kingva1e site. See Table 2.1 for details of the <br />sampling. The samples were collected during the field season at intervals <br />of five to twenty minutes in duration depending on precipitation rate., <br /> <br />All samples from HALO were to be analyzed for their 180 enrichment. <br />A preliminary group of fifteen (15) samples collected during the first <br />experimental unit conducted 7 February 1985 (2050h-2320h GMT) underwent <br />immediate processing into reaction tubes at the DRI laboratories. This <br />is the first step in converting oxygen in the snow samples into carbon <br />dioxide gas from which the 180/160 ratios are determined by mass spectro- <br />metry. The raw data from these initial samplings were discussed at the <br />May 1985 SCPP workshop in Auburn, California. <br /> <br />Selections were made of those samples to be analyzed for indications <br />of silver iodide seeding material and special tracer content. TWo special <br />tracers were used during the 1984-85 studies. The first, cesium (Cs), was <br />released from the seeder aircraft in flares containing CSI03 which produced <br />specially tagged ice nuclei (AgI'CsI). The second, indium (In), was released <br />from the ground-based generator located at Cisco Butte. The program in- <br />volves the analysis of two hundred (200) element-determinations. Therefore, <br />sixty-six (66) samples were to be analyzed each for silver (Ag), cesium (Cs) <br />and indium (In) contents. <br /> <br />I <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br />I <br /> <br />I <br /> <br />I <br />I <br /> <br />1- <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br />I <br /> <br />I <br /> <br />I <br />I <br />