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<br />------------------- <br /> <br />Collision <br /> <br />---------> <br /> <br />t1,T1,F1 <br /> <br />Condensation <br /> <br />------------> <br /> <br />t1,T1,SWl,F2 <br /> <br />Deposition <br /> <br />----------> <br /> <br />t1,T1,Si,F3 <br /> <br />NUCLEATION MODES <br /> <br />O :~~:::~~~>O <br />t1,T1,F1i <br />Freezing <br /> <br />::~~:!~?_> ~ <br /> <br />t2,T2,Flif ~ <br /> <br />---------> <br /> <br />~ <br /> <br />t1,T1,F1f <br /> <br />· Hydrate <br />o Haze particle <br />c.:51ution Drop <br /> <br />Immersion <br /> <br />0.. :::::~~?-> ~ <br /> <br />t2,T2,F2if~ <br /> <br />------------> <br /> <br />t1,T1,SW1,F2i <br /> <br />.po <br />lJ1 <br /> <br />Freezing <br /> <br />~. <br /> <br />------------> <br /> <br />t1,T1,SW1,F2f <br /> <br />o <br /> <br />Figure 4.1 Schematic diagram of the mechanisms by which ice crystals <br />can form in a cooling cloud parcel. Ice particles are <br />indicated by shading and the various symbols describing <br />rates and nucleating fractions are discussed in the text. <br />