. Compendium of meteorology. Meteorology. Fig. 7.—Frost crystal structure produced by surface prop- erty of a solid surface: (a) crystal forms on clean glass, and (6) crystal forms on glass coated with a very thin layer of a dichlorosilane. dropped into cold air supersaturated with respect to ice produce many millions of ice crystals, as shown in Fig. 8. Photomicrographs of such crystals are shown in. Fig. S.—Snow crystals forming in a cold chamber with air supersaturated with respect to ice. Fig. 9. It can easily be shown that 1 g of dry ice may generate 10'* ice crystals under such condition
. Compendium of meteorology. Meteorology. Fig. 7.—Frost crystal structure produced by surface prop- erty of a solid surface: (a) crystal forms on clean glass, and (6) crystal forms on glass coated with a very thin layer of a dichlorosilane. dropped into cold air supersaturated with respect to ice produce many millions of ice crystals, as shown in Fig. 8. Photomicrographs of such crystals are shown in. Fig. S.—Snow crystals forming in a cold chamber with air supersaturated with respect to ice. Fig. 9. It can easily be shown that 1 g of dry ice may generate 10'* ice crystals under such conditions [26]. The critical temperature which produces this effect may be determined in a simple manner. By solidifying. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original American Meteorological Society. Committee on the Compendium of Meteorology; Malone, Thomas F. Boston : American Meteorological Society
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