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<br />~I <br />I <br />I <br />I <br />I <br />.1 <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 />5 <br /> <br />Sec1:ion VI. <br /> <br />It.-Band Radar Measurement aDd Analvsis Proqra!! <br /> <br />This radar, built at DRI, was desiqnt!d to operate in the vert1.cal- <br />pointinq mode at a hiqh mountain site in lfinter. <br /> <br />It usually operated alonqside a microwave radiometer used to measure <br />liquid water and water vapor in approximately the same beam coverage reqions <br />as the radar. 'ftle back-scattered radiatic)D of the Ka radar yielded valuable <br />information, as time series displays, on c::loud base and cloud-top heiqhts, <br />chanqes in reflec1:ivity and band structure in the cloud systellUl. 'l:'he bands <br />could be either wverticalw precipitation reqions movinq across the reqion, <br />or whorizontalW layers representinq preciJ~itation-sized particulates at <br />several levels in the cloud mass. <br /> <br />The proqram supported upqrades and mc)difications to the radar system <br />itself includinq color-displays and sophilsticated data acquisition and <br />storaqe systems. <br /> <br />Both winter seasons covered by the C()ntract yielded val\lable data <br />which has been analyzed and reported in o)nferences and workshops. Probably <br />the most valuable contributions the radar has made to this proqram are: (a) <br />to identify reqions of precipitation qrowth, particularly in the lower cloud <br />reqions over the mountainous terrain, and (b) to define the c~loud base and <br />top elevations continuously throuqhout tht! observing' periods, enablinq <br />reasonable estimates to be made of the concentrations of liq\llid water in <br />the cloud, based on the inteqrated radiomt!ter measurements. Details of <br />individual case studies are qiven in the text of Section VI. <br />