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    A Simulation of the Wangara Atmospheric Boundary Layer Data

    Source: Journal of the Atmospheric Sciences:;1975:;Volume( 032 ):;issue: 012::page 2309
    Author:
    Yamada, Tetsuji
    ,
    Mellor, George
    DOI: 10.1175/1520-0469(1975)032<2309:ASOTWA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Previously, the authors have studied a hierarchy of turbulent boundary layer models, all based on the same closure assumptions for the triple turbulence moments. The models differ in complexity by virtue of a systematic process of neglecting certain of the tendency and diffusion terms in the dynamic equations for the turbulent moments. Based on this work a Level 3 model was selected as one which apparently sacrificed little predictive accuracy, but which afforded considerable numerical simplification relative to the more complex Level 4 model. An earlier paper had demonstrated that the model produced similarity solutions in near agreement with surface, constant flux data. In this paper, simulators from the Level 3 model are compared with two days of Wangara atmospheric boundary layer data (Clarke et al., 1971). In this comparison, there is an easily identified error introduced by our inability to include advection of momentum in the calculation since these terms were not measured. Otherwise, the calculated results and the observational data appear to he in close agreement.
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      A Simulation of the Wangara Atmospheric Boundary Layer Data

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4152801
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    contributor authorYamada, Tetsuji
    contributor authorMellor, George
    date accessioned2017-06-09T14:18:35Z
    date available2017-06-09T14:18:35Z
    date copyright1975/12/01
    date issued1975
    identifier issn0022-4928
    identifier otherams-16960.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4152801
    description abstractPreviously, the authors have studied a hierarchy of turbulent boundary layer models, all based on the same closure assumptions for the triple turbulence moments. The models differ in complexity by virtue of a systematic process of neglecting certain of the tendency and diffusion terms in the dynamic equations for the turbulent moments. Based on this work a Level 3 model was selected as one which apparently sacrificed little predictive accuracy, but which afforded considerable numerical simplification relative to the more complex Level 4 model. An earlier paper had demonstrated that the model produced similarity solutions in near agreement with surface, constant flux data. In this paper, simulators from the Level 3 model are compared with two days of Wangara atmospheric boundary layer data (Clarke et al., 1971). In this comparison, there is an easily identified error introduced by our inability to include advection of momentum in the calculation since these terms were not measured. Otherwise, the calculated results and the observational data appear to he in close agreement.
    publisherAmerican Meteorological Society
    titleA Simulation of the Wangara Atmospheric Boundary Layer Data
    typeJournal Paper
    journal volume32
    journal issue12
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1975)032<2309:ASOTWA>2.0.CO;2
    journal fristpage2309
    journal lastpage2329
    treeJournal of the Atmospheric Sciences:;1975:;Volume( 032 ):;issue: 012
    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