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Last modified
7/28/2009 2:40:22 PM
Creation date
4/24/2008 2:48:46 PM
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Weather Modification
Title
The Persistence of Seeding Effects in a Winter Orographic Cloud Seeded with Silver Iodide Burned in Acetone
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<br />seedline penetrations are also show~. Note that the ascent of the seeding <br /> <br />. '- <br />- '! 'J> I -; <br /> <br />material between 61 and 92 min parallels the slope of the barrier. <br /> <br />The ascent <br /> <br />.1 ; <br /> <br />.J-. <br /> <br />rate of the seeding material was 0.2 m S-1 from the time of release out to 92 <br /> <br />. _"IIi <br />.-- \.. <br /> <br />min. Also show~ in Fig. 30 are predictions from a trajectory model used by ,- <br /> <br />ro. <br /> <br />the SGPP (Rauber et al., 1988). <br /> <br />Predicted trajectories of ice crystals <br /> <br />,. <br /> <br />. . <br /> <br />nucleated 5, 15, 30, and 45 min afLer release of seeding material are shown. <br /> <br />,'. <br /> <br />These predictions of fallout gave an average advection of seeding material to <br /> <br />\ <br /> <br />the surface of 2330 at 12 m S-1 which is 6 m S-1 slower than the advection <br /> <br />", <br /> <br />~ <br /> <br />measured by the aircraft at 3.0 km. The trajectory calculation indicated that <br /> <br />I. <br /> <br />ice crystals would begin reaching the surface after 60 min. Yith this <br /> <br />) 1'_' <br /> <br />advection the southern end of the seedline crossed 3 precipitation gauges, but <br /> <br />passed to the north of KGV. For all three gauges intermittent precipitation <br /> <br />of 1 rr~ h-1, the minim~T. detectable signal, was obsePJed during the time of <br /> <br />" ~ <br />,. I' <br />..."" . <br /> <br />seedline passage. Thus there was no indication in the surface data of the <br /> <br />i-~ rJiL..-- <br /> <br />effects of seeding. <br /> <br />~--- <br /> <br />4. S~~ary and Conclusions <br /> <br />l~ <br /> <br />------ <br /> <br />I cJ <br />L- <br /> <br />J <br /> <br />~'i_J <br />'.~ r- <br /> <br />One line of AgI NH~I NH4Cl04 was released at -60G in a stable post <br /> <br />. I <br />_. i} .,J. <br />frontal stratiform cloud with naLural particle concentrations in excess of 50 .\~:~r>..:(J:- <br /> <br /> <br />L< on the 2D-C. The research ai:::-craft was able to track this seedline to the \~:,,:\.}-, <br />.--It' l~ 'I r ~.", <br />.......~ .:. ~ \.... 't'--u '" ..--/ <br />dow~wind edge of cloud, some 100 km and 92 min after seeding. During irrtttal <br /> <br />penetrations of the seedline high cor.centrations of ice nuclei were measured, <br /> <br />but changes in particle concent:::-ation on the 2D-G or 2D-P were difficult to <br /> <br />!_-- <br /> <br />"- ~ .....,- <br /> <br />... _ ,: _ : ..1.f; <br /> <br />separate from the background. The seedline then apparently ascended above the <br /> <br />research aircraft. No ice nuclei were detected on penetrations between 19 and <br /> <br />61 min. Cpon clinbing the seeding material was again detected wi:h the ice <br /> <br />nacleus counter during penetrations between 64 and 92 min after seeding. The <br /> <br />- 10 - <br />
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