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    Microstructure of a Radiation Fog

    Source: Journal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 002::page 454
    Author:
    Gerber, H. E.
    DOI: 10.1175/1520-0469(1981)038<0454:MOARF>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The relative humidity, temperature, droplet size distribution and transmittance of light at 632.8 nm were measured in a radiation fog. A new saturation hygrometer capable of measuring relative humidity between ?95 and 105%, was used for the first time. Excursions of relative humidity into the supersaturation regime were brief and rapid. Estimated peak values of supersaturation were several tenths of 1%. The mean relative humidity in the fog was <100%. The importance of turbulence in controlling the fog was evident in the rapid fluctuations in all the measured variables, and in the fog's quasi-periodic oscillations which had a mean period of 18 min. Evidence suggested that turbulent mixing of nearly saturated eddies was the cause of fog formation and the broadening of the droplet size distribution.
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      Microstructure of a Radiation Fog

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    contributor authorGerber, H. E.
    date accessioned2017-06-09T14:22:09Z
    date available2017-06-09T14:22:09Z
    date copyright1981/02/01
    date issued1981
    identifier issn0022-4928
    identifier otherams-18093.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4154060
    description abstractThe relative humidity, temperature, droplet size distribution and transmittance of light at 632.8 nm were measured in a radiation fog. A new saturation hygrometer capable of measuring relative humidity between ?95 and 105%, was used for the first time. Excursions of relative humidity into the supersaturation regime were brief and rapid. Estimated peak values of supersaturation were several tenths of 1%. The mean relative humidity in the fog was <100%. The importance of turbulence in controlling the fog was evident in the rapid fluctuations in all the measured variables, and in the fog's quasi-periodic oscillations which had a mean period of 18 min. Evidence suggested that turbulent mixing of nearly saturated eddies was the cause of fog formation and the broadening of the droplet size distribution.
    publisherAmerican Meteorological Society
    titleMicrostructure of a Radiation Fog
    typeJournal Paper
    journal volume38
    journal issue2
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1981)038<0454:MOARF>2.0.CO;2
    journal fristpage454
    journal lastpage458
    treeJournal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 002
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian