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WMOD00376
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Last modified
7/28/2009 2:36:59 PM
Creation date
4/16/2008 10:28:52 AM
Metadata
Fields
Template:
Weather Modification
Contract/Permit #
14-06-D-5640
Project Name
Park Range Atmospheric Water Resources Program
Title
Park Range Atmospheric Water Resources Program - Phase II - Parts A and B
Date
10/6/1967
Weather Modification - Doc Type
Report
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<br />I <br /> <br />I <br /> <br />I <br /> <br />An initial inspection of the first seeding period would indicate that <br />winds are from the wrong direction, but examination of the origina.l data <br />from Emerald Mountain shows a wind shift from 190 to 310 degrees occur- <br />red just after 0100 MST. Perfect alignment of the Emerald and Me Harris <br />11,000 ft. winds is not nece s sary for pulsing to be detected at Rabbit Ear s. <br />Mt. Harris winds of 250 to 360 degrees, with proper Emerald winds (270- <br />3500) have given pulse s at Rabbit Ears, <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />The next simplest case occurs when Emerald Mountain is under an <br /> <br />inversion; it was found during 22% of the observation times, In Figure 14, <br /> <br />an inversion is definitely present as indicated by the moderate westerlies <br /> <br />I <br /> <br />at 11, 000 ft. and the light southe rlie s (changing to northerly) at Emerald. <br /> <br />I <br /> <br />The interesting point is that the nuclei concentration is on the order of <br /> <br />1 per liter during periods of no seeding. Evidently, some of the seeding <br /> <br />agent doe s reach the counter at Rabbit Ear s even when the top of an in- <br /> <br />version is between Emerald Mountain and Rabbit Ears Pass elevationso <br /> <br />I <br /> <br />When the IlK ft. MSL wind from Mt. Harris is between 270 and 360 <br /> <br />I <br /> <br />degrees, the nuclei count usually ran 1-2 nuclei per liter; when that wind <br />was between 180 and 270 degrees, the count was less than, 8e,} per liter. <br /> <br />I <br /> <br />I <br /> <br />Another type of nuclei concentration variation is shown in Figure <br />15, An inversion exists up to about 1230 hours on 25 January, but then <br />there was a wind shift and speed increase at Emerald -- indicating a <br />dissipation of the inversion. High nuclei concentrations were subse- <br /> <br />I <br /> <br />quently measured between 1310 and 1600, This suggests that high con- <br /> <br />I <br /> <br />centrations of ice nuclei were built up under the inversion, and were <br /> <br />released during the first few hours after the stable layer was destroyedo <br /> <br />I <br /> <br />The most difficult case to explain occurred during 18% of the ob- <br />servation times, Both Mt. Harris and Enlerald winds are favorable for <br /> <br />I <br /> <br />detection, but the nuclei concentration rer.nains near 1 per liter, This <br /> <br />case is demonstrated in Figure 16 where, the winds above ridge level are <br /> <br />I <br /> <br />I <br /> <br />- 33 - <br />
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