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    Variability of Local Structure Parameters in the Convective Boundary Layer

    Source: Journal of the Atmospheric Sciences:;2009:;Volume( 066 ):;issue: 004::page 1002
    Author:
    Cheinet, Sylvain
    ,
    Siebesma, A. Pier
    DOI: 10.1175/2008JAS2790.1
    Publisher: American Meteorological Society
    Abstract: The propagation of optical and acoustical waves is affected by the atmospheric turbulence through the local instantaneous refractive index structure parameter in a volume of characteristic size r, denoted Cn,r2. Often r is well within the inertial?convective range. In this study, a large-eddy simulation (LES) of spatial resolution ? is used to analyze the distribution of Cn,?2 in the convective boundary layer. The local formulation used to calculate Cn,?2 is described and is found to back up the subgrid parameterization of atmospheric LES. The mean vertical profile behaves according to the mixed layer similarity theory. The spatial organization relates to the presence of buoyant ascending plumes. This structure is associated with some bimodal probability density functions of the inertial?convective range variables, in agreement with experimental results. The standard model of jointly lognormal statistics is challenged. The intermittency of these variables is characterized, and its inertial?convective range component quantitatively agrees with experimental estimates. The present LES results are used to document the bias produced by averaging the dissipation rates of TKE and temperature variance to estimate the average structure parameters. Comparing with nonconvective turbulence measurements, the bias for CT,r2 is found to depend on the stability. A physical explanation is offered that emphasizes the role of the large-scale turbulence under convective conditions.
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      Variability of Local Structure Parameters in the Convective Boundary Layer

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    contributor authorCheinet, Sylvain
    contributor authorSiebesma, A. Pier
    date accessioned2017-06-09T16:23:00Z
    date available2017-06-09T16:23:00Z
    date copyright2009/04/01
    date issued2009
    identifier issn0022-4928
    identifier otherams-66875.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4208259
    description abstractThe propagation of optical and acoustical waves is affected by the atmospheric turbulence through the local instantaneous refractive index structure parameter in a volume of characteristic size r, denoted Cn,r2. Often r is well within the inertial?convective range. In this study, a large-eddy simulation (LES) of spatial resolution ? is used to analyze the distribution of Cn,?2 in the convective boundary layer. The local formulation used to calculate Cn,?2 is described and is found to back up the subgrid parameterization of atmospheric LES. The mean vertical profile behaves according to the mixed layer similarity theory. The spatial organization relates to the presence of buoyant ascending plumes. This structure is associated with some bimodal probability density functions of the inertial?convective range variables, in agreement with experimental results. The standard model of jointly lognormal statistics is challenged. The intermittency of these variables is characterized, and its inertial?convective range component quantitatively agrees with experimental estimates. The present LES results are used to document the bias produced by averaging the dissipation rates of TKE and temperature variance to estimate the average structure parameters. Comparing with nonconvective turbulence measurements, the bias for CT,r2 is found to depend on the stability. A physical explanation is offered that emphasizes the role of the large-scale turbulence under convective conditions.
    publisherAmerican Meteorological Society
    titleVariability of Local Structure Parameters in the Convective Boundary Layer
    typeJournal Paper
    journal volume66
    journal issue4
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/2008JAS2790.1
    journal fristpage1002
    journal lastpage1017
    treeJournal of the Atmospheric Sciences:;2009:;Volume( 066 ):;issue: 004
    contenttypeFulltext
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