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<br />. <br /> <br />. <br /> <br />Karacostas, Theodore S., TUrbulent dlrtu~ionstudies or winter storms <br />over the Sierra N~vada MOuntains, Ph. D., <br />Department of Atmospheric Science, University <br />of Wyoming, December, 1981. <br /> <br />. <br /> <br />The Lagrangian Turbulent Diffusion (LTD) model is developed, criti- <br /> <br />. <br /> <br />cally evaluated and applied over the Sierra Nevada Mountains. The data <br /> <br />were co llec ted in the course 0 f the Bureau 0 f Rec lama t ion's Sierra Coope- <br /> <br />rative Pilot ProJect (SCPP) in the field seasons 1977-78, 1978-79, and <br /> <br />. <br /> <br />1979-80. <br /> <br />The statistical theory was used as the basic theoretical framework <br /> <br />for the development of the model, which expresses the complex process of <br /> <br />. <br /> <br />turbulent diffusion as an analytical equation. The LTD model describes <br /> <br />the time his tory' 0 f the seeding ma ter ia I as they wander through the flow <br /> <br />. <br /> <br />field, and g:ives a fundamentally correct picture of the actual mechanism <br /> <br />of turbulent d iffus ion. <br /> <br />It is shown theoretically and experimentally <br /> <br />that the LTD' model is an appropriate method to predict the diffusion of <br /> <br />. <br /> <br />a seeded plume for diffusion times longer than the characteristic time <br /> <br />associated with the most energetic eddies. <br /> <br />. <br /> <br />The important assumptions and hypotheses used in the development of <br /> <br />the LTD model are validated theoretically and experimentally. Procedures <br /> <br />for adopting aircraft measurements to the LTD model are developed and the- <br /> <br />. <br /> <br />oretically evaluated. The Taylor's frozen-turbulence hypothesis is shown <br /> <br />. <br />