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<br />4 <br /> <br />I <br />I <br />I <br />I <br />I <br />1 <br />I <br />I <br />1 <br />I <br />I <br />I <br />1 <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />The purpose of this dissertation is to describe the physical structure <br /> <br />and temporal evolution of the wintertime cloud systems which occur over <br /> <br /> <br />the Northern Colorado River Basin. The specific objectives of this <br /> <br /> <br />research are to: (1) relate the physical structure of the cloud systems <br /> <br />over the region to the large scale environment in which they form; (2) <br /> <br />determine the physical distribution, temporal variation, microphysical <br /> <br /> <br />structure and climatological frequency of supercooled water; (3) examine <br /> <br />the physical processes associated with the development of the ice phase, <br /> <br /> <br />specifically, primary nucleation, ice multiplication, vapor deposition, <br /> <br /> <br />accretion and aggregation; (4) develop a coherent physical model of the <br /> <br /> <br />natural precipitation process in these clouds and (S) assess, <br /> <br /> <br />qualitatively, the potential of weather modification to augment <br /> <br /> <br />precipitation in this region. <br /> <br /> <br />This document is of considerable length. Chapter II contains a <br /> <br /> <br />disoussion of instrumentation. Chapters III and IV contain analyses of <br /> <br /> <br />liquid and ice phase processes respectively. Chapter V presents a <br /> <br /> <br />summary of the material in the previous two chapters. For those readers <br /> <br /> <br />not wishing to examine the detailed analyses, Chapter V is a concise <br /> <br /> <br />synopsis of this material in this thesis. Chapter VI contains a <br /> <br /> <br />qiscussion of precipitation augmentatiOn hypotheses and experiments and <br /> <br />Chapter VII summarizes the major conolusions. <br /> <br /> <br />1. Back2ro)Jnd <br /> <br /> <br />Weather modification research programs utilize three methods to <br /> <br /> <br />evaluate the results of experiments. The first method, statistical <br /> <br /> <br />analysis, uses randomization procedures over a sufficient data sample to <br /> <br /> <br />insure that a change in precipitation, if it exists, oan be recognized <br /> <br /> <br />. as. a statistically significant effect.. The precipitation data are, then <br /> <br />