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<br />I <br /> <br />30 <br /> <br />I <br /> <br />1000 <br /> <br />1000 <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />;::-100 - 0 0 <br />... 0 100 - <br />~ 0 0 0 <br /> 0 0 00 6'0 <br />2 0 .. <br />0 .... <br /> 0 ~ <br />f- 0 <br />ct <br />a: 0 0 0 <br />f- <br />2 Z <br />W 0 <br />u 10 0 0 00 ~- <br />2 0 ~ 10 <br />0 0 0::: <br />U f- <br /> 00 2 <br />-.J Lu 00\ <br />~ 0 U <br /> '? <br /> c_ <br />~ 0 <br /> u <br />a: <br />u 0 -.J <br /> 0 <:! <br />w I- <br />U U) <br /> >- <br /> - 0 n:: <br /> I u I - <br /> lJJ <br /> U <br /> <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />0./ I I <br /> , I <br />-20 -10 0 -20 -10 0 <br /> TEMPERATURE (C) TEMPERATURE (C) <br /> a b <br /> <br /> <br />I <br /> <br />I <br /> <br />Figure 3.4. (a) lee crystal concentration as a function of the temperature <br />at which the concentration \vas observed, for a set of observa- <br />tions with no selection criteria except that the observation <br />point be well within the cloud. <br />(b) Same as (a), except only those observations are included for <br />which a clear origin for the crystals was determined. Concentr:'- <br />tions are plotted as a function of the temperature at \vhich the <br />cloud f:in;t fanned, ,~ather than the temperature at the point of <br />observation. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br />