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<br />Section 2. - RADAR <br /> <br />The Utah State Universi ty Ka-band radar was llsed for data collection from <br />November 17, 1984 through April 30, 1985. <br /> <br />The radar was co-located with the USU Microwave Radiometer at Island Lake <br />on the Grand Mesa. Coordinates were 39002115" N., l0800QI17"W. and about <br />3,172 m (10,400 ft.) altitude ms.l. <br /> <br />The major characteristics of thE~ radar are outlined in table 2-1. The <br />antenna was positioned in a vertically pointing orientation. The data was <br />recorded on facsimile paper whenever the radar was set to transmit. A <br />16-mm time-exposure, time-lapse camera photographed an oscilloscope that <br />functioned as an A.-scope. Photographs were once every 5 mi nutes con- <br />tinuously, 24 hours per day, whE~ther the radar was operating or not. The <br />output product is a vertical profile of reflectivity against time. <br /> <br />Dates of useful photography (backup purposes only) are December 5, 1984 to <br />January 9, 1985, and January 16, 1985 to April 5, 1985. <br /> <br />Dates of radar data collection on facsimile paper are listed in table 2-2. <br /> <br />These data will be reduced to provide computer files containing the <br />following information for each hour with echoes present: <br /> <br />1. Average precipitation tops for the hour, and a coded representation <br />of the precipitation type (stratiform, convective, etc.) <br /> <br />2. Maximum precipitation top observed within the hour and a coded repre- <br />sentation of the precipitation type (stratiform, convective, etc.) <br /> <br />These data will be available on magnetic tape approximately June 15, 1985. <br /> <br />2-1 <br />