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<br />which report activation of ice crystals following silver iodide seeding for <br />15 min. and longer. <br /> <br />Seeding agents such as silver iodide-sodium iodide and silver iodide- <br />potassium iodide which appear to act by the consdensation-freezing mode of <br />nucleation have somewhat shorter nucleation time constants. Blumenstein <br />et al. (1983) report that a silver iodide-sodium iodide nucleant produces 90 <br />percent of its ice crystals in about 14 to 20 min. depending on <br />temperature, in a cloud chamber at water saturation. However, when sub- <br />jected to transient supersaturations with respect to water, both the <br />nucleation rate and effectivity of the nucleant increased. In super- <br />saturated conditions this nucleant produced 90 percent of its ice crystals <br />in about 4 min. and its effectivity increased by almost one order of magni- <br />tude. Rilling et al. (1984) found that a silver iodide-potassium iodide <br />nucleant behaves similarly. Finnegan et al. (1984) showed that the incor- <br />poration of a hygroscopic salt, .like sodium chloride, into the silver <br />iodide-silver chloride nucleus composition changed its mode of nucleation <br />from contact to condensation-freezing, thereby increasing both its effec- <br />tivity and nucleation rate, especially under transient supersaturation con- <br />ditions. <br /> <br />The combined effects of a silver iodide seeding agent's nucleation rate and <br />residence time in a cloud is to make the nucleant's ice crystal yield less <br />than its effectivity at all temperatures, the amount of reduction depending <br />on the mode of nucleation and thE~ cloud conditions where and when <br />nucleation actually occurs. In effect it lowers the temperature threshold <br />of activity for most silver iodide seeding agents to about _90 to -10 oc. <br /> <br />21 <br />