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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 />6.31 Experiment (symbols) and equivalent model simulation 184 <br />(lines) cumulative ice formation versus temperature for <br />several in-cloud seeding experiments with AgI-AgCl <br />aerosols. Injections of 0.03~m aerosols (experiments 7288, <br />5787, 2589) are shown in plots (a) to (c), while 0.07~m <br />aerosol injections (experiments 7188, 2689) are shown in <br />-1 <br />plots (d) and (e). Equivalent expansion updraft is 2.5 m s . <br /> <br />6.32 As in Figure 6.3l, but for AgI-AgCl-4NaCl aerosols. Panels 185 <br />(a) to (c) are for 0.03~m aerosol injections (experiments <br />8088, 3689, 3489), and panels (d) to, (f) are for 0.07~m <br />aerosol injections (experiments 8188, 6188, 3589). <br /> <br />6.33 Model (solid lines) versus experimental (dashed lines) 189 <br />thermodynamic and cloud quantities in warm cloud base <br />seeding experiment using polydisperse AgI-AgCl aerosols <br />-1 <br />experiment 7488). Equivalent expansion updraft is 2.5 m s . <br /> <br />6.34 Cumulative (+) and differential (0) F values observed and 190 <br />those predicted by new model formulations (lines) in clouds <br />seeded before formation near OOC with 0.03~m (a), 0.07~m <br />(b), and polydisperse (c) AgI-AgCl aerosols. Cooling rate <br />is approximately lOC min-1 for these 2.5 m s-l ascent <br />simulations (experiments 7688, 7588, 7488). <br /> <br />6.35 As in Figure 6.34, but for 0.03~m (a), 0.7pm (b), and 19l <br />polydisperse (c) AgI-AgCl-4NaCl aerosols (experiments 7988, <br />6488, 6688). <br /> <br />6.36 Comparison of contributions of various nucleation modes to 192 <br />ice formation by polydisperse AgI-AgCl (a) and AgI-AgC1- <br />4NaCl (b) aerosols seeded before the formation of cloud at <br />OOC. <br /> <br />6.37 Model thermodynamic and cloud quantities for simulation of 196 <br />below-cloud seeding of an orographic cloud with AgI-AgCl <br />aerosols. The ice signal is given L-1. The initial parcel <br />4 -1 <br />concentrations were 10 L . A panel for average maximum <br />crystal dimension is included with the quantities <br />previously displayed for cloud chamber simulations. <br /> <br />6.38 Comparison of cumulative ice fractions formed versus 197 <br />temperature in orographic seeding simulation using AgI-AgCl <br />aerosols or AgI-AgCl-4NaCl aerosols. <br /> <br />6.39 Model thermodynamic and cloud quantities for simulation of 199 <br />below cloud seeding of a summertime cumulus cloud with AgI- <br />AgCl aerosols. Parcel initial conditions and updraft <br />characteristics are described in the text. <br /> <br />xu <br />