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    Evaluation of Large-Eddy Simulations via Observations of Nocturnal Marine Stratocumulus

    Source: Monthly Weather Review:;2005:;volume( 133 ):;issue: 006::page 1443
    Author:
    Stevens, Bjorn
    ,
    Moeng, Chin-Hoh
    ,
    Ackerman, Andrew S.
    ,
    Bretherton, Christopher S.
    ,
    Chlond, Andreas
    ,
    de Roode, Stephan
    ,
    Edwards, James
    ,
    Golaz, Jean-Christophe
    ,
    Jiang, Hongli
    ,
    Khairoutdinov, Marat
    ,
    Kirkpatrick, Michael P.
    ,
    Lewellen, David C.
    ,
    Lock, Adrian
    ,
    Müller, Frank
    ,
    Stevens, David E.
    ,
    Whelan, Eoin
    ,
    Zhu, Ping
    DOI: 10.1175/MWR2930.1
    Publisher: American Meteorological Society
    Abstract: Data from the first research flight (RF01) of the second Dynamics and Chemistry of Marine Stratocumulus (DYCOMS-II) field study are used to evaluate the fidelity with which large-eddy simulations (LESs) can represent the turbulent structure of stratocumulus-topped boundary layers. The initial data and forcings for this case placed it in an interesting part of parameter space, near the boundary where cloud-top mixing is thought to render the cloud layer unstable on the one hand, or tending toward a decoupled structure on the other hand. The basis of this evaluation consists of sixteen 4-h simulations from 10 modeling centers over grids whose vertical spacing was 5 m at the cloud-top interface and whose horizontal spacing was 35 m. Extensive sensitivity studies of both the configuration of the case and the numerical setup also enhanced the analysis. Overall it was found that (i) if efforts are made to reduce spurious mixing at cloud top, either by refining the vertical grid or limiting the effects of the subgrid model in this region, then the observed turbulent and thermodynamic structure of the layer can be reproduced with some fidelity; (ii) the base, or native configuration of most simulations greatly overestimated mixing at cloud top, tending toward a decoupled layer in which cloud liquid water path and turbulent intensities were grossly underestimated; (iii) the sensitivity of the simulations to the representation of mixing at cloud top is, to a certain extent, amplified by particulars of this case. Overall the results suggest that the use of LESs to map out the behavior of the stratocumulus-topped boundary layer in this interesting region of parameter space requires a more compelling representation of processes at cloud top. In the absence of significant leaps in the understanding of subgrid-scale (SGS) physics, such a representation can only be achieved by a significant refinement in resolution?a refinement that, while conceivable given existing resources, is probably still beyond the reach of most centers.
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      Evaluation of Large-Eddy Simulations via Observations of Nocturnal Marine Stratocumulus

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4228928
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    contributor authorStevens, Bjorn
    contributor authorMoeng, Chin-Hoh
    contributor authorAckerman, Andrew S.
    contributor authorBretherton, Christopher S.
    contributor authorChlond, Andreas
    contributor authorde Roode, Stephan
    contributor authorEdwards, James
    contributor authorGolaz, Jean-Christophe
    contributor authorJiang, Hongli
    contributor authorKhairoutdinov, Marat
    contributor authorKirkpatrick, Michael P.
    contributor authorLewellen, David C.
    contributor authorLock, Adrian
    contributor authorMüller, Frank
    contributor authorStevens, David E.
    contributor authorWhelan, Eoin
    contributor authorZhu, Ping
    date accessioned2017-06-09T17:26:54Z
    date available2017-06-09T17:26:54Z
    date copyright2005/06/01
    date issued2005
    identifier issn0027-0644
    identifier otherams-85477.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4228928
    description abstractData from the first research flight (RF01) of the second Dynamics and Chemistry of Marine Stratocumulus (DYCOMS-II) field study are used to evaluate the fidelity with which large-eddy simulations (LESs) can represent the turbulent structure of stratocumulus-topped boundary layers. The initial data and forcings for this case placed it in an interesting part of parameter space, near the boundary where cloud-top mixing is thought to render the cloud layer unstable on the one hand, or tending toward a decoupled structure on the other hand. The basis of this evaluation consists of sixteen 4-h simulations from 10 modeling centers over grids whose vertical spacing was 5 m at the cloud-top interface and whose horizontal spacing was 35 m. Extensive sensitivity studies of both the configuration of the case and the numerical setup also enhanced the analysis. Overall it was found that (i) if efforts are made to reduce spurious mixing at cloud top, either by refining the vertical grid or limiting the effects of the subgrid model in this region, then the observed turbulent and thermodynamic structure of the layer can be reproduced with some fidelity; (ii) the base, or native configuration of most simulations greatly overestimated mixing at cloud top, tending toward a decoupled layer in which cloud liquid water path and turbulent intensities were grossly underestimated; (iii) the sensitivity of the simulations to the representation of mixing at cloud top is, to a certain extent, amplified by particulars of this case. Overall the results suggest that the use of LESs to map out the behavior of the stratocumulus-topped boundary layer in this interesting region of parameter space requires a more compelling representation of processes at cloud top. In the absence of significant leaps in the understanding of subgrid-scale (SGS) physics, such a representation can only be achieved by a significant refinement in resolution?a refinement that, while conceivable given existing resources, is probably still beyond the reach of most centers.
    publisherAmerican Meteorological Society
    titleEvaluation of Large-Eddy Simulations via Observations of Nocturnal Marine Stratocumulus
    typeJournal Paper
    journal volume133
    journal issue6
    journal titleMonthly Weather Review
    identifier doi10.1175/MWR2930.1
    journal fristpage1443
    journal lastpage1462
    treeMonthly Weather Review:;2005:;volume( 133 ):;issue: 006
    contenttypeFulltext
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