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    Relationship between the Vertical Velocity Skewness and Kurtosis Observed during Sea-Breeze Convection

    Source: Journal of Applied Meteorology:;2002:;volume( 041 ):;issue: 008::page 885
    Author:
    Alberghi, S.
    ,
    Maurizi, A.
    ,
    Tampieri, F.
    DOI: 10.1175/1520-0450(2002)041<0885:RBTVVS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Fourth-order moments of vertical velocity in the convective boundary layer (CBL) are seldom available because the unsteady nature of atmospheric flows makes time statistics unreliable for the evaluation of high-order moments. In this paper, sound detection and ranging (sodar) measurements in well-developed, almost steady convective conditions are selected and analyzed to investigate the relationship between skewness and kurtosis. Moments of vertical velocity up to the fourth order are computed with special attention to the assessment of the errors connected to the number of independent data and to the inherent spatial and temporal filtering of the measuring system. Results show that a significant correlation between skewness and kurtosis exists in the lower half of the CBL, and a quadratic relationship is proposed that is similar to the one valid for alongwind velocity in shear-dominated boundary layers.
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      Relationship between the Vertical Velocity Skewness and Kurtosis Observed during Sea-Breeze Convection

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4148593
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    contributor authorAlberghi, S.
    contributor authorMaurizi, A.
    contributor authorTampieri, F.
    date accessioned2017-06-09T14:08:31Z
    date available2017-06-09T14:08:31Z
    date copyright2002/08/01
    date issued2002
    identifier issn0894-8763
    identifier otherams-13172.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4148593
    description abstractFourth-order moments of vertical velocity in the convective boundary layer (CBL) are seldom available because the unsteady nature of atmospheric flows makes time statistics unreliable for the evaluation of high-order moments. In this paper, sound detection and ranging (sodar) measurements in well-developed, almost steady convective conditions are selected and analyzed to investigate the relationship between skewness and kurtosis. Moments of vertical velocity up to the fourth order are computed with special attention to the assessment of the errors connected to the number of independent data and to the inherent spatial and temporal filtering of the measuring system. Results show that a significant correlation between skewness and kurtosis exists in the lower half of the CBL, and a quadratic relationship is proposed that is similar to the one valid for alongwind velocity in shear-dominated boundary layers.
    publisherAmerican Meteorological Society
    titleRelationship between the Vertical Velocity Skewness and Kurtosis Observed during Sea-Breeze Convection
    typeJournal Paper
    journal volume41
    journal issue8
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(2002)041<0885:RBTVVS>2.0.CO;2
    journal fristpage885
    journal lastpage889
    treeJournal of Applied Meteorology:;2002:;volume( 041 ):;issue: 008
    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