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Okita, T. (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
Observations of the vertical structure of radiation fogs and a stratus cloud were made by means of a rotary droplet sampler and other techniques. The results of the surveys of four radiation fogs and one stratus cloud are presented. It is found that the upper part of a deep fog or a stratus cloud has a similar physical structure to a cumulus cloud. The observation reveals that ordinary fog droplets grow mainly by condensation. It is also found that the presence of large droplets of radii about 50 microns or more near the top of the fog or stratus cloud is a necessary condition for the production of drizzle. The rate of growth of the large droplets is approximately explained by the Langmuir's accretion theory.DOI: 10.1111/j.2153-3490.1962.tb01342.x
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    • FINDEISENW, ., 1932, Messungen der Grosse und Anzahl der Nebeltropfen zum Studium der KoagulationinhomogenenNebels, Beitr. Geophys., 86, p. 295
    • FLEAQLRE., G., PARROTWT,. H., and BARADM,. L., 1953, Theory and effects of vertical temperature distribution in turbid air. Journ. Met., 9, p. 53.
    • HANAJIMAM,., 1945, Measurements of total water content and liquid water content in fog. study of Fog in Chishima and Hokkaido, No. 26 (in Japanese).
    • HOWELLW,. E., 1949, The growth of cloud drops in uniformly cooled air. Journ. Met., 6 , p. 134.
    • KINZERG, . D., and COBB,W. E., 1958, Laboratory meaeurements and analysis of the growth and collection efficiency of cloud droplets. Journ. Met., 16, p. 138.
    • KRAUSE,. B., and SMITE,S., 1949, Theoretical aspects of cloud drop distributions. Australian Journ. Sci. Res., 2, p. 376.
    • L A N G M ~IR.,,1948, The production of rain by a chain reaction in cumulus clouds of temperatures above freezing. Journ. Met., 6 , p. 175.
    • MORDY,W., 1959, Computations of the growth by condensation of a population of cloud droplets. Tellua, 11,p. 16.
    • OWCHI,H., 1949, On the method of the measurement of the size and number of fog droplets. Low Temperature Science, 2 , p. 105 (in Japanese).
    • OKITA, T., 1958, Water-blue film method for measurement of cloud and fog droplets. Journ. Met. SOC.Japan, 31, p. 237.
    • OKITA,T., 1961, Size distribution of large droplets in precipitating clouds. Tellus, 13, p. 509.
    • SCHUYANNT., E. W., 1940, Theoretical aspects of the size distribution of fog particles. Quart. Journ. Roy.Met. SOC.,66, p. 195.
    • TAKAHASHYI,., 1952, Sea fog of advection type over Oyashio. Seventh Pacific Science Congress, 3, p. 1.
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