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contributor authorFukuta, N.
date accessioned2017-06-09T14:14:56Z
date available2017-06-09T14:14:56Z
date copyright1969/05/01
date issued1969
identifier issn0022-4928
identifier otherams-15611.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4151303
description abstractThe fall velocities and growth rates of freely falling ice crystals were measured at various intervals for about 1 min after ice crystal nucleation of a supercooled fog. Measurements were also made at various degrees of supercooling. The results showed that: 1) the velocity varied linearly with time t for 60 sec after the first 12-sec period, with two falling velocity plateaus being found at ?5 and ?8, and ?10 and ?18C; 2) the mass varied as t1/2 except at ?18 to ?19C, a small mass growth rate peak being found at ?6.5C; 3) the larger peak shifted toward colder regions as the crystal grew; 4? tsuzumi crystals formed at around ?18C; and 5) at the temperatures where two maxima of the mass growth occurred, the apparent densities were at minima. Current theory failed to describe the mass growth rate of ice crystals. The existence of an unknown factor was detected and introduced into the rate equation of ice crystal growth.
publisherAmerican Meteorological Society
titleExperimental Studies on the Growth of Small Ice Crystals
typeJournal Paper
journal volume26
journal issue3
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1969)026<0522:ESOTGO>2.0.CO;2
journal fristpage522
journal lastpage531
treeJournal of the Atmospheric Sciences:;1969:;Volume( 026 ):;issue: 003
contenttypeFulltext


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