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o!! limi ted analyses of these important clouds has been complE!ted. These blanket type orographic clouds, which produced nearly half of the precipitation, were not seen by the C-band radar and were not probed by the aircraft. However, it is expected that analyses based on rawinsonde, radiometer, mountaintop, and precipitation observations can provide very useful descriptions of these important d.ouds. 2. Area-wide cloud systems produced about 20% of the precipitation during the field program. The results of the Feburary 8 case study showed that, for at least this area-wide cloud, the majority of the observations of supercooled liquid water were limited to the low level, upwind portions of the cloud. When this saturated air underwent substantial lifting near the Tushar crest, additional significant supercooled liquid water could have been produced. This has been substantiated to some degree by surface measurements. No substantial amounts of liquid water were observed in the mid and upper level cloud regions. Thus, at lower levels, these area-wide clouds may have some characteristics similar to those in the blanket orographic clouds. It appears that these neutral and stable type, clouds, including the blanket orographic clouds (around 50%) and the area-,~ide clouds (around 20%) produced about 70% of the precipitation during the field program. ~, .. ~ 3. Convective clouds produced about one-third of the precipitation during the field experiment. At least some of these cellular type clouds had substantial amounts of supercooled liquid water that was not converted to precipitation over the Tushar Mountains. This was particularly true during the 28 F'eb 1983 storm system when substantial liquid water contents were observed and virtually no precipitation occurred. .. iii