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<br />I <br />I <br /> <br />I <br /> <br />~ <br />o <br />M <br /> <br />I <br /> <br />I <br />I <br />I <br /> <br />I <br />I <br />I <br />I <br /> <br />~ <br />o <br />M <br /> <br />o <br />w <br />~ <br /><< <br />W <br />~ <br />U <br />~ <br />Z <br />Z <br />o <br />H <br />~ <br />U <br />.<< <br />~ <br />~ <br /> <br />I <br /> <br />I <br />I <br /> <br />I <br />I <br />I <br /> <br />35 <br /> <br />10 <br /> <br />x <br /> <br />o <br />w <br />~ <br /><< <br />W <br />~ <br />U <br />~ <br />Z <br />Z <br />o <br />H <br />~ <br />U <br /><< <br />~ <br />~ <br /> <br />8 <br /> <br />. <br /> <br />6 <br /> <br /> <br />4 <br /> <br />2 <br /> <br />o <br /> <br />-16 <br /> <br />-12 <br /> <br />-8 <br /> <br />-4 <br /> <br />TEMP (OC) <br /> <br />10 <br /> <br />x <br /> <br />8 <br /> <br /> <br />b <br /> <br />6 <br /> <br />4 <br /> <br />2 <br /> <br />~ <br /> <br />o <br /> <br />-16 <br /> <br />-12 <br /> <br />-8 <br /> <br />-4 <br /> <br />TEMP (OC) <br /> <br />Figure 3.6 Example of the result of applying the deconvolution <br />procedure to real experimental data. The raw (lines) and <br />smoothed (- + -) numbers of crystals settling from the <br />cloud (per s) as a fraction of ice nucleus aerosols <br />injected versus temperature are shown in (a). The <br />deconvo1uted and smoothed-deconvoluted signals are given in <br />(b). <br /> <br />I <br /> <br />I <br />