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<br />. <br /> <br />. <br /> <br />Prasad, N. <br /> <br />Precipitation lDeve10pment in Seeded Clouds over <br />the Sierra Nevada <br />M.S., Department of Atmospheric Science, <br />August, 1986. <br /> <br />- <br /> <br />. <br /> <br />The Sierra Cooperative pilot Project is a weather modification <br /> <br />experiment in the Sierra Nevada of Central California. During the <br /> <br />winter months 1977-1986 (except 1981) orographica11y-induced <br /> <br />. <br /> <br />convective clouds and stratifonn clouds with isolated and anbedded <br /> <br />convection, respectively, were seeded with dry ice and silver <br /> <br />iodide. Their response to seeding was investigated. <br /> <br />.e <br /> <br />The particle growth model of Heymsfie1d (1982) anbedded in a <br /> <br />kinematic flow field repl:esentative of the Sierra barrier was used <br /> <br />to study the ice particle growth by diffusion, accretion and <br /> <br />. <br /> <br />subsequent fall trajecJcories. <br /> <br />The particles observed by the <br /> <br />aircraft were classified into habits. <br /> <br />The growth of observed <br /> <br />particles were compared with the model predicted evolution. Using <br />"-~ <br /> <br />.e <br /> <br />an aggregation model of Heymsfie1d (1986), the observation of <br /> <br />formation of aggregates in < 10 minutes was verified. <br /> <br />The key <br /> <br />findings of this research were: <br /> <br />(1) Diffusional growth is <br /> <br />i. <br /> <br />extremely important for temperatures near -lSoC in these low <br /> <br />liquid water content clouds. <br /> <br />The particles grow to "'2 mn when <br /> <br />e <br /> <br />released from just colder than -lSoC, and to "'1 TIm when falling <br /> <br />from warmer than -lSoC. (2) Riming is important close to the <br /> <br />barrier in a stratiform cloud when large cloud droplets and liguid <br /> <br /> <br />~ater up to 0.3 g m-3 cl~e present. (3) Aggregates (> 1 rrm) form in <br />4-8 minutes after seeding a convective cloud. <br /> <br />. <br /> <br />. <br /> <br />. <br />I <br />