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<br />1 <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 /> <br />I. Introduction <br /> <br />The continuing research under the cooperative Atmospheric Modification Research <br />Program (AMP) between the National Oceanic and Atmospheric Administration (NOAA) <br />and the state of Utah included a winter field program from 15 January through 15 March <br />1994. The emphasis of this program on the Wasatch Plateau in central Utah was the <br />documentation of the transport and dispersion of silver iodide (Agl) cloud seeding <br />aerosols from ground-based generators. The Utah Department of Water Resources <br />(UDWR, 1994) described the,plan for the field program which included participation by <br />numerous other agencies, including the Desert Research Institute (DRI). <br />The DRI participated in a number of the 1994 field activities including mobile <br />microwave radiometer operations, Ka-Band radar operations, rawinsonde operations, the <br />collection of time sequential snow samples for analysis of silver, the archiving of pertinent <br />satellite and synoptic weather data, and the deployment of two remotely-controlled <br />generators for dispensing Agl. These activities were aimed at describing the spatial <br />distribution of supercooled cloud liquid as in Huggins (1994), describing the spatial <br />distribution of cloud ice from scanning radar data, and verifying the presence of cloud <br />seeding material in snowfall at the project's primary target site. Radar data are also <br />expected to contribute to transport and dispersion studies through the analysis of radar <br />returns resulting from chaff being released from seeding generator sites. The upper air <br />soundings were used to provide initiation input for the mesoscale modeling aspect of the <br />program (Heimbach, 1993), as well as data for deriving atmospheric retrieval coefficients <br />for microwave radiometric data and important information on the stability of the <br />atmosphere during the release of seeding material. The 1994 NOAA/Utah project area <br />and primary instrumentation sites are shown in Fig. 1. <br />Overall the DRI work contributed to the scientific objectives of the NOAA/Utah <br />Project, which are: 1) to describe the spatial and temporal distributions of supercooled <br />liquid water (SLW) in winter clouds over Utah's mountains and the factors controlling <br />the SLW; 2) to understand how silver iodide cloud seeding material may be delivered <br />from ground generators to the winter cloud regions containing SLW; 3) to gain a better <br />