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<br />4.1 Schematic diagram of the mechanisms by which ice crystals <br />can form in a cooling cloud parcel. "Ice particles are <br />indicated by shading and the various symbols describing <br />rates and nucleating fractions are discussed in the text. <br /> <br />4.2 Schematic of the thermodynamic history of a parcel between <br />ice and water saturation (a) during expansion-cooling, <br />representing a pathway over which deposition nucleation can <br />be measured. Computation of the nucleation rate at two <br />points is shown in (b). <br /> <br />4.3 Dry particle size versus equivalent haze particle size of <br />AgI-AgCl-4NaCl aerosols at water saturation, computed <br />empirically as described in the text. <br /> <br />4.4 Size distribution of AgI-AgCl aerosols from the CSU standard <br />generator, determined by scanning electron microscopy. <br /> <br />4.5 Size distribution of AgI-AgCl-4NaCl aerosols produced by <br />the CSU standard generator, determined by electrostatic <br />classification. The double hatched distribution gives the <br />raw measurements, while the single hatched area is the <br />distribution after correction for charging efficiency and <br />multiple charging effects (see text). <br /> <br />5.1 Ice formation with respect to cloud formation point in two <br />experiments used in the analysis of deposition nucleation <br />by AgI-AgC1 aerosols. The raw ( )and deconvo1uted ( ) ice <br />-1 <br />fractions nucleated (s ) versus temperature are shown in <br />part (a). Cloud droplet concentrations ( ) are also <br />indicated. The deconvo1uted cumulative ice fractions <br />nucleated are compared versus ice supersaturation in part <br />(b). Cloud formation points are indicated by arrows. <br /> <br />5.2 Summary of the thermodynamic history of data records <br />indicating ice formation before cloud point in a number of <br />experiments used to quantify deposition nucleation for AgI- <br />AgCl (a) and AgI-AgCl-4NaC1 aerosols. <br /> <br />5.3 Active site density by deposition versus supersaturation <br />with respect to ice for AgI-AgCl aerosols. A power law fit <br />to the data using (5.1) is indicated. Data points are coded <br />to be lOO times the aerosol diameter in microns. <br /> <br />5.4 Fractions of AgI-AgCl aerosols effective by deposition for <br />AgI-AgCl aerosols. Points are coded as in Figure 5.3, and <br />the lines through the crosses indicate values computed for <br />0.07 and 0.03~m diameter sizes using (5.1). <br /> <br />xii <br /> <br />45 <br /> <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 />48 <br /> <br />53 <br /> <br />64 <br /> <br />65 <br /> <br />67 <br /> <br />69 <br /> <br />70 <br /> <br />71 <br />