Laserfiche WebLink
<br />described by Huggins (1990) and Huggins and Sass en (1990). As with the 199() study, <br />the chemical analysis determined that snowfall at the selected target did not contain <br />silver above background for a significant percentage of the seeding periods. These <br />results lead to changes in experimental approach in NOAA/Utah and to the set of <br />seeding experiments that were conducted in 1994. <br />During the 1994 field program, snow samples were captured at TAR in a 1.2 m <br />diameter collection cylinder covered with clean plastic. Field technicians removed the <br />snow from the cylinder at intervals of 10 to 30 minutes, depending on snowfall rate, <br />transferred the snow to clean plastic bags, labeled the bags and stored them in an ice <br />chest at TAR until the end of an experiment. The samples from all experiments were <br />stored in a freezer at field headquarters. Table 6 documents the days and time periods <br />during which samples were collected at TAR. Of the 10 days on which samples were <br />taken, six have sufficient samples to resolve temporal changes during the experiments. <br />Following the field program all of the samples were taken back to DRI in a freezer <br />transported by the mobile radiometer. To date the samples have been prepared for <br />chemical analysis. The specific sample times, the mass of snow in each sample and the <br />computed precipitation rate for each sample time period are contained in Appendix B. <br /> <br />25 <br /> <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 />