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<br />ACKNOWLEDGEMEN'l'S <br /> <br />The author wishes to e~press appreciation to his supervisors, Dr T L Clark and <br />Dr A J Heymsfield of the National Center for Atmospheric Research (NCAR) in <br />Boulder, Colorado, for their invaluable advice and encouragement tl1roughout <br />this study. I would like to express my appreciation to the Weather Bureau in <br />the Department of Environment Affairs, the Water Research Commission and the <br />University of Arizona who sponsored my visit to NCAR to wor~ on the research <br />discussed in this thesis. Specifically I would like to thank Mr P S du Toit <br />of the Weather Bureau and Dr R Gall of the University of Arizona who on <br />numerous occassions provided valuable encouragement and ideas regarding this <br />study. Special thanks should go to Dr W Hall of NCAR who provided special <br />guidance in getting myself acquainted with the numerical model. NCAR deserves <br />special acknowledgement. in providing the computer resources and administrative <br />support. The numerous interactions with other NCAR and University of Arizona <br />staff proved to be extremely stimulating and helpful during the course of the <br />research. I also wish to thank Sudy Kelly and Paula Parsley for their efforts <br />in making my stay at NCAR most enjoyable. <br /> <br />The staff of the National Program for Precipitation Research in South Africa <br />and the Bureau of Reclamation in the USA are acknowledged for the collection <br />of the observational data used in the research. Suzette Pienaar, Cindy <br />Bruyere and Nico Kroese are specifically thanked for their help in the final <br />preparation of the figures and the text. <br /> <br />Finally I would like to express my sincere appreciation to my wife Roelie and <br />children for their continued support, having to make many sacrifices by <br />travelling with me on many occasions during the past ten years. <br /> <br />""0 <br /> <br />SOLI DEO GLORIA <br /> <br />I.. <br /> <br />"! <br /> <br /># <br /> <br />. <br /> <br />. <br /> <br />. <br />