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<br />I <br />I. <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />- 75 - <br /> <br />Definition of Symbols <br /> <br />x, z Coordinates of horizontal and vertical directions. <br /> <br />z Vertical location at x = - m of streamline passing <br />o <br />through (x, z). <br /> <br />Vertical separations between two streamlines at x = <br /> <br />3.4.l <br /> <br />tJ.z, tJ.z <br />o <br /> <br />x and <br /> <br />x = - 00. <br /> <br />u, u <br />o <br /> <br />Horizontal wind components at (x, z) and (_m, z ), <br />o <br />respectively. <br /> <br />Vertical wind component at (x, z). <br /> <br />Slope of streamline at (x, z). <br /> <br />Temperatures at (x, z) and (_m, z ), respectively. <br />o <br />Liquid water contents at (x, z) and (-~, z ), respectively. <br />o <br />Specific heat of dry air at constant pressure. <br /> <br />Collection efficiency. <br /> <br />Height of cloud base. <br /> <br />Mass of ice particle. <br /> <br />Radius of ice particl~ <br /> <br />Time. <br /> <br />Time increment in calculating increase in mass of ice <br /> <br />particle. <br />Terminal velocities of ice crystals and cloud droplets, <br />respectively. . <br />Temperature lapse ~ates of dry air and saturated air, <br />respectively. <br />Concentration of ice particles. <br /> <br />Critical concentration of ice particles. <br /> <br />w <br />tan ~ <br />T, T <br /> 0 <br />X, X <br /> 0 <br />c <br />P <br />E <br />H <br />c <br />M <br />r <br />t <br />tJ.t <br /> <br />Vc' Vd <br /> <br />Yd' Ym <br /> <br />N <br />o <br />N <br />c <br /> <br />