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<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 />I <br />I <br />I <br />I <br />I <br />I <br /> <br /> <br />~ <br /> <br /> <br />~ ~ <br />s\ <br />~\ <br />\ <br />I <br />j <br /> <br />? <br /> <br />i\ <br />\ <br /> <br />v <br /> <br />HQ <br />D <br /> <br /> <br />o 2 3 4 5 e 7 8 II 10 K__ <br />i I I I I I I I I <br /> <br />SCALE <br /> <br />Figure J. i.'vfap of the 1994 UtahNOAAfield research area on the Wasatch Plateau of central Utah. <br />Ka-band radar. USBR radiometer. meteorological station and NCAR counter were located at RRS. <br />PiHS 2-DC probe. meteorological station. NCAR counter and snow sampling equipment were <br />located at TAR Doppler acoustic sounder was at DAS. Silver iodide seeding generators. propane <br />generators and SF6 release equipment were at HAS and AHS. Precipitation gages were located at <br />points marked P. Arfobile radiometer was located at HQ, and was driven across plateau on <br />Highways 31 and 264. Terrain contours are in meters. <br /> <br />starting altitudes was used for all of the data. A.constant adjustment was then applied to force the <br />liquid values to zero when an offset above or below zero (typically <0.03 mm) was ob"ious in <br />cloudless conditions. The same retrieval coefficients were used for both the DRI mobile radiometer <br /> <br />4 <br />