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    The Critical Richardson Number and Its Implications for Forecast Problems

    Source: Journal of Applied Meteorology:;1964:;volume( 003 ):;issue: 002::page 136
    Author:
    Lyons, Richard
    ,
    Panofsky, H. A.
    ,
    Wollaston, Sarah
    DOI: 10.1175/1520-0450(1964)003<0136:TCRNAI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: It is shown that, in the lowest few hundred meters, nighttime inversions tend to break down due to onset of turbulence when the Richardson number falls between 0.2 and 0.5. Since the Richardson number is statistically related to the wind speed at one to a few hundred meters, it is found that the dew-point depression in the morning, as well as visibility, is related to the wind speed above the surface. It follows, that objective forecast techniques for the dew-point depression and visibility can be improved by including the wind speed above the surface as a parameter.
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      The Critical Richardson Number and Its Implications for Forecast Problems

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4212389
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    • Journal of Applied Meteorology

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    contributor authorLyons, Richard
    contributor authorPanofsky, H. A.
    contributor authorWollaston, Sarah
    date accessioned2017-06-09T16:35:39Z
    date available2017-06-09T16:35:39Z
    date copyright1964/04/01
    date issued1964
    identifier issn0021-8952
    identifier otherams-7059.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4212389
    description abstractIt is shown that, in the lowest few hundred meters, nighttime inversions tend to break down due to onset of turbulence when the Richardson number falls between 0.2 and 0.5. Since the Richardson number is statistically related to the wind speed at one to a few hundred meters, it is found that the dew-point depression in the morning, as well as visibility, is related to the wind speed above the surface. It follows, that objective forecast techniques for the dew-point depression and visibility can be improved by including the wind speed above the surface as a parameter.
    publisherAmerican Meteorological Society
    titleThe Critical Richardson Number and Its Implications for Forecast Problems
    typeJournal Paper
    journal volume3
    journal issue2
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1964)003<0136:TCRNAI>2.0.CO;2
    journal fristpage136
    journal lastpage142
    treeJournal of Applied Meteorology:;1964:;volume( 003 ):;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
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