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<br />I <br />I <br /> <br />25 <br /> <br />19 <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />I <br />5 <br /> <br />J <br />J <br /> <br />9 <br /> <br /> <br />u <br />0 <br />- T <br /> -5 d J <br />a. J <br />1: <br />W <br />.... <br /> J <br /> -19 <br /> <br /> <br />-I <br />I <br />I <br />! <br />~ <br />~ <br />-l <br />J <br />I <br />...J <br />j <br />i <br />~ <br />! <br />1 <br />.., <br />I <br />-l <br />I <br />-' <br />I <br />-< <br /> <br />-15 <br /> <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />-29 <br /> <br />499 <br /> <br />475 <br /> <br />669 <br /> <br />626 <br /> <br />799 <br /> <br />PRESSURE (mb) <br /> <br />Figure 3.2 <br /> <br />An example of a programmed (T versus P) versus the <br />simulated ascent profile experime~tally observed (T versus <br />P) in the dynamic cloud chamber. Dewpoint temperature as <br />measured by the optical condensation-type hygrometer is <br />also shown. <br /> <br />I <br /> <br />I <br />