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    Vertical Variations of Mixing Lengths under Neutral and Stable Conditions during CASES-99

    Source: Journal of Applied Meteorology and Climatology:;2011:;volume( 050 ):;issue: 010::page 2030
    Author:
    Sun, Jielun
    DOI: 10.1175/JAMC-D-10-05006.1
    Publisher: American Meteorological Society
    Abstract: n investigation on vertical variations of the mixing lengths for momentum and heat under neutral and stable conditions was conducted using the data collected from the Cooperative Atmosphere?Surface Exchange Study in 1999 (CASES-99). By comparing ?z with the mixing lengths under neutral conditions calculated using the observations from CASES-99, the vertical layer where the Monin?Obukhov similarity theory (MOST) is valid was identified. Here ? is the von Kármán constant and z is the height above the ground. On average, MOST is approximately valid between 0.5 and 10 m. Above the layer, the observed mixing lengths under neutral conditions are smaller than the MOST ?z and can be approximately described by Blackadar?s mixing length, ?z/[1 + (?z/l∞)], with l∞ = 15 m for up to z ~ 20 m for the mixing length for momentum and up to the highest observation height for the mixing length for heat. Above ~20 m, the mixing length for momentum approaches a constant. Both MOST ?z and Blackadar?s formula systematically overestimate the mixing length for momentum above ~20 m, leading to overestimates of turbulence.
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      Vertical Variations of Mixing Lengths under Neutral and Stable Conditions during CASES-99

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4216724
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    contributor authorSun, Jielun
    date accessioned2017-06-09T16:48:25Z
    date available2017-06-09T16:48:25Z
    date copyright2011/10/01
    date issued2011
    identifier issn1558-8424
    identifier otherams-74493.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4216724
    description abstractn investigation on vertical variations of the mixing lengths for momentum and heat under neutral and stable conditions was conducted using the data collected from the Cooperative Atmosphere?Surface Exchange Study in 1999 (CASES-99). By comparing ?z with the mixing lengths under neutral conditions calculated using the observations from CASES-99, the vertical layer where the Monin?Obukhov similarity theory (MOST) is valid was identified. Here ? is the von Kármán constant and z is the height above the ground. On average, MOST is approximately valid between 0.5 and 10 m. Above the layer, the observed mixing lengths under neutral conditions are smaller than the MOST ?z and can be approximately described by Blackadar?s mixing length, ?z/[1 + (?z/l∞)], with l∞ = 15 m for up to z ~ 20 m for the mixing length for momentum and up to the highest observation height for the mixing length for heat. Above ~20 m, the mixing length for momentum approaches a constant. Both MOST ?z and Blackadar?s formula systematically overestimate the mixing length for momentum above ~20 m, leading to overestimates of turbulence.
    publisherAmerican Meteorological Society
    titleVertical Variations of Mixing Lengths under Neutral and Stable Conditions during CASES-99
    typeJournal Paper
    journal volume50
    journal issue10
    journal titleJournal of Applied Meteorology and Climatology
    identifier doi10.1175/JAMC-D-10-05006.1
    journal fristpage2030
    journal lastpage2041
    treeJournal of Applied Meteorology and Climatology:;2011:;volume( 050 ):;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
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