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<br />. <br /> <br />. <br /> <br />ACKNOWLEDGMENTS <br /> <br />.' <br /> <br />The author is deeply indepted to and wishes to acknowledge his dis- <br /> <br />.. <br /> <br />sertation advisor, Dr. John D. MBrwitz, tor his valuable suggestions, con- <br /> <br />tinual patience and invaluable guidance from the initial planning to the <br /> <br />f ina I wr it ing of this research,' His input ot ideas into the organiza Hon <br /> <br />.i <br /> <br />of this dissertation as well as the editing, proofreading, and supplying <br /> <br />innumerable grammatical and wording improvements, proved invaluable. He <br /> <br />. <br /> <br />was of particular help and made the writing easier with his routinely <br /> <br />prompt reading of the rough dratts, and that was deeply appreciated. The <br /> <br />many stimulating discussions with Dr. MBrwitz were an outstanding part of <br /> <br />. <br /> <br />the author's graduate studies at the Department ot Atmospheric Science of <br /> <br />the University of Wyoming. Dr. MBrwitz has given freely of his time and <br /> <br />ideas, ans has had a maJor influence in developing the author's attitudes <br /> <br />. <br /> <br />regarding education and science. <br /> <br />The author is also deeply indepted to Dr. William R. Lindberg, ot <br /> <br />. <br /> <br />the Department of Mechanical Engineering, for his guidance, encouragement <br /> <br />and his constant willingness to discuss turbulent diffusion theory and <br /> <br />its application to this study; <br /> <br />. <br /> <br />. <br />