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<br />Experiment 3: Spatial and temporal distribution of supercooled <br />liquid water <br /> <br />Lead Scientist: Alexis B. Long, DRI <br /> <br />Participating Scientists: <br /> <br />Patricia A. Walsh, DRI <br />Jack B. Snider, WPL <br />Robert M. Rauber, CSU <br />Norihiko Fukuta, Kenneth Sassen, UU <br />Thomas J. Henderson, AI <br /> <br />Objectives of the analysis are 1) to describe the spatial distribu- <br /> <br />tion and temporal variation of supercooled liquid water in clouds in the <br /> <br />vicinity of the WPL radiometer and to relate this information to <br /> <br />orographic features of the Tushar Mtns, 2) to measure the height and <br /> <br />from this calculate the temperature of the liquid water in clouds above <br /> <br />the Iidar, and 3) to intercompare supercooled liquid water detector <br /> <br />data, surface microphysics observations, radiometer data, and Iidar <br /> <br />information on liquid water. <br /> <br />The analysis leading to the first objective will be based in part <br /> <br />on contoured plots of liquid water depth as a function of azimuth and <br /> <br />time for groups of radiometer azimuth scans made during important <br /> <br />segments of STORMS. <br /> <br />Interpretation of the plots will consider <br /> <br />orographic features, the direction and speed of ambient flow over the <br /> <br />mountains, and the convective or stratiform nature of the clouds. <br /> <br />Radiometer data collected in the elevation scan mode will also be ana- <br /> <br />Iyzed. <br /> <br />The data will first be normalized for slant path length of the <br /> <br />radiometer field of view. <br /> <br />Interpretations will then be made as to how <br /> <br />the liquid water amount varies with pos!~tion upwind and over the Tushar <br /> <br />Mtns. The radiometer data for individual STORMS will be appropriately <br /> <br />composited to yield a picture of the liquid water distribution for the <br /> <br />entire field program. <br /> <br />28 <br /> <br />., <br /> <br />.- <br /> <br />. <br /> <br />. <br /> <br />i. <br /> <br />410 --.' <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br />