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    Surface layer Similarity under Nonuniform Fetch Conditions

    Source: Journal of Climate and Applied Meteorology:;1983:;volume( 022 ):;issue: 010::page 1800
    Author:
    Beljaars, A. C. M.
    ,
    Schotanus, P.
    ,
    Nieuwstadt, F. T. M.
    DOI: 10.1175/1520-0450(1983)022<1800:SLSUNF>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: This paper discusses the results of a surface-layer experiment near the Cabauw meteorological mast. We measured momentum, heat and moisture fluxes at two heights, namely, 3.5 and 22.5 m. The measurements also include the mean wind speed and mean temperature profiles. The purpose was to investigate surface-layer similarity laws under nonideal fetch conditions. We found that under such conditions, the shell stress increases with height because of obstacles upstream. As a consequence flux-profile relationships differ from those over uniform terrain. It is shown that these deviations imply a slow relaxation in the exchange coefficient for heat and momentum over a terrain with changing surface roughness. Furthermore, we found that horizontal velocity fluctuations scale on a friction velocity representative of a large area. On the other hand, vertical velocity fluctuations scale on the local friction velocity.
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      Surface layer Similarity under Nonuniform Fetch Conditions

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4145737
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    contributor authorBeljaars, A. C. M.
    contributor authorSchotanus, P.
    contributor authorNieuwstadt, F. T. M.
    date accessioned2017-06-09T13:59:49Z
    date available2017-06-09T13:59:49Z
    date copyright1983/10/01
    date issued1983
    identifier issn0733-3021
    identifier otherams-10601.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145737
    description abstractThis paper discusses the results of a surface-layer experiment near the Cabauw meteorological mast. We measured momentum, heat and moisture fluxes at two heights, namely, 3.5 and 22.5 m. The measurements also include the mean wind speed and mean temperature profiles. The purpose was to investigate surface-layer similarity laws under nonideal fetch conditions. We found that under such conditions, the shell stress increases with height because of obstacles upstream. As a consequence flux-profile relationships differ from those over uniform terrain. It is shown that these deviations imply a slow relaxation in the exchange coefficient for heat and momentum over a terrain with changing surface roughness. Furthermore, we found that horizontal velocity fluctuations scale on a friction velocity representative of a large area. On the other hand, vertical velocity fluctuations scale on the local friction velocity.
    publisherAmerican Meteorological Society
    titleSurface layer Similarity under Nonuniform Fetch Conditions
    typeJournal Paper
    journal volume22
    journal issue10
    journal titleJournal of Climate and Applied Meteorology
    identifier doi10.1175/1520-0450(1983)022<1800:SLSUNF>2.0.CO;2
    journal fristpage1800
    journal lastpage1810
    treeJournal of Climate and Applied Meteorology:;1983:;volume( 022 ):;issue: 010
    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