Abstract
This study describes the growth modes of polyhedral ice crystals grown from spherical ice crystals formed by freezing of supercooled water droplets. Frozen water droplets were grown on a thin glass plate at -15 and -7°C and at humidities above and below water saturation. In the case of growth at -15°C and at a humidity above water saturation, a frozen water droplet grows into an 8-faced ice crystal through a 20-faced ice crystal, while in the case of growth at -15°C and at a humidity between the ice saturation and the water saturation, it grows into an 8-faced ice crystal with truncated edges and corners through an 8-faced ice crystal with curved and flat surfaces. The growth modes at -7°C and at humidities above and below water saturation are almost the same as those at -15°C, except that the axial ratios c/a of the droxtals at -15°C are about 0.95 but those at -7°C are about 1.04.
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