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<br />.. <br /> <br />the detection of a signal over the Tushars and also increase the <br /> <br />opportunity to receive a weak stgnal needs to be considered. <br /> <br />6. Special attention needs to be directed toward obtaining cloud physics <br /> <br />aircraft data in the upper portions of the blanket orographic clouds. <br /> <br />Ku-band radar data shows that this is feasible. <br /> <br />7. The need for surface observations is great. These are essential for <br /> <br />describing the snow crystal tYPE~S, ice particle evaluation (riming,. <br /> <br />aggregation, etc.), trajectories and concentrations for the lower <br /> <br />portions of the clouds that cannot be sampled either by aircraft <br /> <br />or mountaintop observations. <br /> <br />'!\ <br /> <br />~ <br /> <br />8. lncreased emphasis needs to be given to more complete, high resolution <br /> <br />observations of mountaintop supercooled liquid water. <br /> <br />9. Continued field observations are needed to provide more precise <br /> <br />descriptions of the respective cloud types and to provide information <br /> <br />on the representativeness of the cloud cases that occurred during the <br /> <br />1982-83 field research program. <br /> <br />~ <br /> <br />.; <br /> <br />v <br />