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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 />Precipitation measurements are made by a network of recording <br /> <br /> <br />precipi ta tion gages. The number of gages has varied from 30 to 60. <br /> <br /> <br />Some of the gages are in remote areas and require servicing by <br /> <br />helicopter. The snowfall at the ground is also studied by the GML <br /> <br /> <br />(ground microphysics laboratory). The GML consists of a camper truck <br /> <br /> <br />equipped with instruments for counting and measuring snow crystals <br /> <br /> <br />and for studying their shapes. In addition, snow samples sometimes <br /> <br />are collected for analysis of trace impurities, including silver, to <br /> <br /> <br />see if changes in precipitation rate can be related to changes in silver <br /> <br /> <br />content in the snow. <br /> <br />A relative newcomer to the SCPP instrumentation list is a dual-channel <br /> <br /> <br />microwave radiometer. This instrument, operated for the past two seasons <br /> <br />at high elevations in the ARB, will be discussed in the next section <br /> <br /> <br />on program results. <br /> <br />3. Results from Physical Observations Within Sierra Storms <br /> <br /> <br />3. 1 Supercooled Liquid Wa ter and its Rela tion to Sierra Nevada <br /> <br /> <br />Meteorology <br /> <br />It is generally agreed that the presence of SLW (supercooled liquid <br /> <br /> <br />water) is a necessary although not always sufficient condition for <br /> <br />precipitation increases to occur due to cloud seeding in winter storms <br /> <br />over mountains. It is therefore necessary to understand the synoptic <br /> <br />and mesoscale controls which determine when supercooled water will <br /> <br />exist over the ARB. Therefore SCPP scientists have given close attention <br /> <br />to the problem of finding and measuring SLW and relating its occurrence <br /> <br />to the meteorological setting. <br /> <br />11 <br />