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<br /> 1.0 <br /> 0.9 <br /> 08 <br />o Q7 <br />I.LJ <br />...J <br />l- <br />I- 0.6 <br />I.LJ <br />C/) <br />z 0.5 <br />0 <br />t> OA <br /><( <br />a: <br />I.L. 0.3 <br /> 02 <br /> 0.1 <br /> 0.0 <br /> 0 10 <br /> <br /> <br />--- ~ ----- --- - <br />..- - -~ ~ ,..- <br />,., ..- ~ ~ /" .......... <br />/' /.,.; ~ /' .................... <br />/'......- ~ /' .......... <br />/'/ /'. ......- <br />// // / . / <br />. // I. / / <br />// / / <br />II / / <br />II I / <br />/ / / <br /> <br />// 1 / / <br />/ ~ / / <br />-ll/-20 o/~,'.!8 1-3 "C <br />/; ~/ / <br />~ /l / // <br />~/ / <br />/' / <br />20 30 40 50 60 70 80 90 100 110 120 130 140 150 160 170 ISO <br />TIME (s) <br /> <br />w <br />.po <br /> <br /> <br />Figure 3.5 Temporal rates of ice crystal formation versus temperature <br />measured following instantaneous nucleation using dry ice. <br />Data are from experiments conducted in the CSU isothermal <br />cloud chamber by Morrison (1989). The solid line is the <br />unit transfer function used in this study. <br /> <br />------------------- <br />