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    Toward Parameterization of the Stable Boundary Layer

    Source: Journal of Applied Meteorology:;1982:;volume( 021 ):;issue: 001::page 7
    Author:
    Wetzel, Peter J.
    DOI: 10.1175/1520-0450(1982)021<0007:TPOTSB>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The bulk Richardson number formula for the depth of the nocturnal boundary layer (NBL) is compared to the Wangara observational data. A correlation of 0.89 is found between the observed NBL depth and the depth calculated using a fixed value of bulk Richardson number. This observed NBL depth is defined as the top of a layer, found consistently in the observations, in which the virtual potential temperature varies linearly with height. The Richardson number expression is also found to be a better estimator of NBL depth, defined in a number of other ways. Based on these findings, a simple three-layer parameterization of the NBL is developed and shown to compare favorably with observations. Within the framework of a prognostic equation for virtual potential temperature, the model diagnoses two important NBL heights, one corresponding to the top of the turbulent layer and the other to the inversion or cooling depth. The single prognostic equation, along with four accompanying diagnostic expressions, also describes the temperature structure of the entire NBL. The model is simple enough to be integrated on a programmable hand calculator.
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      Toward Parameterization of the Stable Boundary Layer

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4145276
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    contributor authorWetzel, Peter J.
    date accessioned2017-06-09T13:58:32Z
    date available2017-06-09T13:58:32Z
    date copyright1982/01/01
    date issued1982
    identifier issn0021-8952
    identifier otherams-10187.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145276
    description abstractThe bulk Richardson number formula for the depth of the nocturnal boundary layer (NBL) is compared to the Wangara observational data. A correlation of 0.89 is found between the observed NBL depth and the depth calculated using a fixed value of bulk Richardson number. This observed NBL depth is defined as the top of a layer, found consistently in the observations, in which the virtual potential temperature varies linearly with height. The Richardson number expression is also found to be a better estimator of NBL depth, defined in a number of other ways. Based on these findings, a simple three-layer parameterization of the NBL is developed and shown to compare favorably with observations. Within the framework of a prognostic equation for virtual potential temperature, the model diagnoses two important NBL heights, one corresponding to the top of the turbulent layer and the other to the inversion or cooling depth. The single prognostic equation, along with four accompanying diagnostic expressions, also describes the temperature structure of the entire NBL. The model is simple enough to be integrated on a programmable hand calculator.
    publisherAmerican Meteorological Society
    titleToward Parameterization of the Stable Boundary Layer
    typeJournal Paper
    journal volume21
    journal issue1
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1982)021<0007:TPOTSB>2.0.CO;2
    journal fristpage7
    journal lastpage13
    treeJournal of Applied Meteorology:;1982:;volume( 021 ):;issue: 001
    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