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<br />. <br /> <br />. <br /> <br />ABSTRACT <br /> <br />. <br /> <br />Experimental data on ice crystal growth measured during recent <br /> <br /> <br />investigations in a supercooled cloud tunnel that suspended ice crystals for <br /> <br /> <br />time periods up to 30 min at the University of Utah have been analyzed. <br /> <br /> <br />These experimental investigations previously generated unique data sets of <br /> <br /> <br />mass, dimensions and fall velocity as a function of time under different <br /> <br /> <br />temperatures and removed some obstacles caused by the tack of proper <br /> <br />experimental data that have hindered cloud microphysical research. <br /> <br /> <br />The analysis in this thesis was set out to fulfill at least the following four <br /> <br /> <br />goals using the data sets from the previous experiments. First, some specific <br /> <br />features of microphysical theories have been verified with the experimental <br /> <br /> <br />data. Second, time . dependent equations of mass, dimensions and fall <br /> <br /> <br />velocity applicable to different ragimes of growth have been developed by <br /> <br /> <br />considering the measured data and the functional styles of theories and not by <br /> <br /> <br />merely obtaining a set of best filting polynomials. Third, an empirical <br /> <br /> <br />equation was derived by similar means to express the aerodynamic behavior <br /> <br /> <br />of the falling ice crystal with the relationship among the Reynolds number, <br /> <br /> <br />the Best number and the axial ratio. Finally, a set of simplified parameterized <br /> <br /> <br />equations has been generated that is experimentally consistent and suitable <br /> <br /> <br />for cloud modeling and analysis. <br /> <br /> <br />The empirical equations generated in this thesis based on the specific <br /> <br /> <br />functional style of the theory have the advantage over the best fit polynomial <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br />