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    On the Reliability of the Parameterization of Microphysics in Fog Models

    Source: Journal of Applied Meteorology:;1979:;volume( 018 ):;issue: 004::page 487
    Author:
    Corradini, C.
    ,
    Tonna, G.
    DOI: 10.1175/1520-0450(1979)018<0487:OTROTP>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The relationships between the mean terminal speed of fog droplets (vE) and the liquid water content (W), and between the integral volume droplet absorption coefficient (σE) and W, have been examined on the basis of 107 experimental fog droplet size spectra selected from the literature, in order to investigate the reliability of parameterizing the microphysics, in fog models, through W. The results show that a weak correlation exists between vE and W, the values of the linear correlation coefficients (R) being 0.12, 0.30, ?0.19 and 0.67, for valley, advection, radiation and artificial fog, respectively. Thus parameterizations of vE through W only are generally unreliable, and other parameterizations, in terms of more than one parameter, should be developed. On the other hand, a good correlation between σE and W has been found, with R = 0.98, 0.87, 0.91 and 0.99 for the fog types indicated above. Comparisons between the values of σE and those obtained by the best-fit lines and by the parameterizations used in fog models, together with the evaluation of the effect of such approximations on the radiative cooling profile, have been carried out.
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      On the Reliability of the Parameterization of Microphysics in Fog Models

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4233197
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    contributor authorCorradini, C.
    contributor authorTonna, G.
    date accessioned2017-06-09T17:39:59Z
    date available2017-06-09T17:39:59Z
    date copyright1979/04/01
    date issued1979
    identifier issn0021-8952
    identifier otherams-9682.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4233197
    description abstractThe relationships between the mean terminal speed of fog droplets (vE) and the liquid water content (W), and between the integral volume droplet absorption coefficient (σE) and W, have been examined on the basis of 107 experimental fog droplet size spectra selected from the literature, in order to investigate the reliability of parameterizing the microphysics, in fog models, through W. The results show that a weak correlation exists between vE and W, the values of the linear correlation coefficients (R) being 0.12, 0.30, ?0.19 and 0.67, for valley, advection, radiation and artificial fog, respectively. Thus parameterizations of vE through W only are generally unreliable, and other parameterizations, in terms of more than one parameter, should be developed. On the other hand, a good correlation between σE and W has been found, with R = 0.98, 0.87, 0.91 and 0.99 for the fog types indicated above. Comparisons between the values of σE and those obtained by the best-fit lines and by the parameterizations used in fog models, together with the evaluation of the effect of such approximations on the radiative cooling profile, have been carried out.
    publisherAmerican Meteorological Society
    titleOn the Reliability of the Parameterization of Microphysics in Fog Models
    typeJournal Paper
    journal volume18
    journal issue4
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1979)018<0487:OTROTP>2.0.CO;2
    journal fristpage487
    journal lastpage494
    treeJournal of Applied Meteorology:;1979:;volume( 018 ):;issue: 004
    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