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<br />. <br /> <br />8 <br /> <br />. <br /> <br />The value of these data can be seen in Fig. 1 where the mass of the <br /> <br /> <br />crystal, grown in the cloud tunnel for 10 minutes, was compared with that <br /> <br /> <br />calculated by Jayaweera (1971) and Miller and Young (1979). The large <br /> <br /> <br />discrepancy between these data and the results of the numerical calculations <br /> <br /> <br />illustrates the space for model improvement. Indeed, most of these models <br /> <br /> <br />are based on previous theories and these experimental data can serve to <br /> <br /> <br />improve the theories. <br /> <br /> <br />Thus, an opportunity is present to improve the theoretical basis in ice <br /> <br /> <br />phase cloud microphysics in comparison with the unique supercooled cloud <br /> <br /> <br />tunnel data of ice crystal growth, and the purpose of this thesis is to make use <br /> <br /> <br />of it. This work will set out to accomplish at least three tasks. First, some <br /> <br /> <br />results of microphysical theory will be verified with experimental data. <br /> <br /> <br />Second, time - dependent equations of mass, a- and c-axial lengths, and fall <br /> <br /> <br />velocity applicable to different regimes of growth will be developed by using <br /> <br /> <br />theories and measured data. Finally, a set of simplified parameterized <br /> <br /> <br />equations will be generated that will be experimentally and theoretically <br /> <br /> <br />consistent and suitable for cloud modeling. <br /> <br /> <br />To accomplish this task, the thesis is divided into six chapters. Chapter 2 <br /> <br /> <br />will discuss the experimental data to be used in this thesis. Chapter 3 is <br /> <br /> <br />designated for development of the time dependent equations for ice crystal <br /> <br />growth parameters. An equation describing the fall behavior of a crystal based <br /> <br /> <br />upon the Reynolds number and habit will be discussed in Chapter 4. A set of <br /> <br /> <br />simplified parameterized equations applicable for cloud modeling will be <br /> <br />derived in Chapter 5. The final chapter will be devoted to summarizing <br /> <br /> <br />results and drawing conclusions. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br />