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Last modified
7/28/2009 2:35:30 PM
Creation date
3/11/2008 2:42:50 PM
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Template:
Weather Modification
Title
Cloud Physics Studies in Utah During 1978
Date
9/1/1978
State
UT
Weather Modification - Doc Type
Report
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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 />and changed directions slightly, moving from the west northwest. On the <br />east side of the Uintas it recurved cyclonically to a west southwest flow. <br />From Figure 4. 1.6c at 3.0 km pressure altitude the flow is seen to be <br />from a westerly direction with speeds from 10 to 15 m s-l and the stream- <br />lines are parallel to the 8 lines. <br />e <br />Figure 4.1.7 contains analog traces of the reverse flow temperature <br />2D-P concentrations, 2D-C concentrations, the liquid water content from the <br />FSSP and the liquid water content from the Johnson-Williams 1 iquid water <br />meter. The period of time when these observations were taken was from <br />1415 to 1421, which occurred during the north to south pass across the <br />center of the Uinta Mountains at a flight altitude of about 4.8 km (See <br />Figure 4.1.5 and 4.1.6a). From this figure it may be seen that the <br />temperature varied between -18 and -190C, the 2D-P concentrations were 10 <br />to 20 t-1 and the 2D-C concentrations were 50 to 100 t-1. The FSSP <br />indicated no substantial 1 iquid water with small concentrations of less than <br />0.1 g m-3 throughout the cloud. A slightly larger amount of liquid water <br />was observed on the northern side of the mountain near 1419. The Johnson- <br />Williams 1 iquid water meter indicated no liquid water except near 1419 <br />when 0.1 9 m-3 was observed. <br />The 2D-images observed from 1418 to 1419 did not show marked changes <br />from regions of high 2D-concentrations to regions of low 2D-concentrations. <br />A typical example of the 2D-images recorded is shown in Figure 4.1.8. <br />Plate-like and stellar-like irregular crystals were the dominant type, and <br />many of these were as large as mm in diameter. There were also a few <br />columns. These were typically < 500 ~m in length and most of them appeared <br />to be unrimed. <br />From the data it is clear that the crystal concentrations were more <br />than adequate to naturally deplete the available liquid water in the cloud. <br />Seeding of the Uinta Range was not attempted nor does it appear that any <br />potential for snow augmentation existed. <br /> <br />21 <br />
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