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    Parameterization of PBL Processes in an Atmospheric General Circulation Model: Description and Preliminary Assessment

    Source: Monthly Weather Review:;2009:;volume( 137 ):;issue: 003::page 1061
    Author:
    Konor, Celal S.
    ,
    Boezio, Gabriel Cazes
    ,
    Mechoso, Carlos R.
    ,
    Arakawa, Akio
    DOI: 10.1175/2008MWR2464.1
    Publisher: American Meteorological Society
    Abstract: This paper presents the basic features of a newly developed planetary boundary layer (PBL) parameterization, and the performance assessment of a version of the University of California, Los Angeles (UCLA), Atmospheric General Circulation Model (AGCM) to which the parameterization is incorporated. The UCLA AGCM traditionally uses a framework in which a sigma-type vertical coordinate for the PBL shares a coordinate surface with the free atmosphere at the PBL top. This framework facilitates an explicit representation of processes concentrated near the PBL top, which is crucially important especially for predicting PBL clouds. In the new framework, multiple layers are introduced between the PBL top and earth?s surface, allowing for predictions of the vertical profiles of potential temperature, total water mixing ratio, and horizontal winds within the PBL. The vertically integrated ?bulk? turbulent kinetic energy (TKE) is also predicted for the PBL. The PBL-top mass entrainment is determined through an equation including the effects of TKE and the radiative and evaporative cooling processes concentrated near the PBL top. The surface fluxes are determined from an aerodynamic formula in which the velocity scale depends both on the square root of TKE and the grid-scale PBL velocity at the lowermost model layer. The turbulent fluxes within the PBL are determined through an approach that includes the effects of both large convective and small diffusive eddies. AGCM simulations with the new formulation of PBL are analyzed with a focus on the seasonal and diurnal variations. The simulated seasonal cycle of stratocumulus over the eastern oceans is realistic, as are the diurnal cycles of the PBL depth and precipitation over land. The simulated fluxes of latent heat, momentum, and shortwave radiation at the ocean surface and baroclinic activity in the middle latitudes show significant improvements over the previous versions of the AGCM based on the single-layer PBL.
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      Parameterization of PBL Processes in an Atmospheric General Circulation Model: Description and Preliminary Assessment

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4209360
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    contributor authorKonor, Celal S.
    contributor authorBoezio, Gabriel Cazes
    contributor authorMechoso, Carlos R.
    contributor authorArakawa, Akio
    date accessioned2017-06-09T16:26:16Z
    date available2017-06-09T16:26:16Z
    date copyright2009/03/01
    date issued2009
    identifier issn0027-0644
    identifier otherams-67866.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4209360
    description abstractThis paper presents the basic features of a newly developed planetary boundary layer (PBL) parameterization, and the performance assessment of a version of the University of California, Los Angeles (UCLA), Atmospheric General Circulation Model (AGCM) to which the parameterization is incorporated. The UCLA AGCM traditionally uses a framework in which a sigma-type vertical coordinate for the PBL shares a coordinate surface with the free atmosphere at the PBL top. This framework facilitates an explicit representation of processes concentrated near the PBL top, which is crucially important especially for predicting PBL clouds. In the new framework, multiple layers are introduced between the PBL top and earth?s surface, allowing for predictions of the vertical profiles of potential temperature, total water mixing ratio, and horizontal winds within the PBL. The vertically integrated ?bulk? turbulent kinetic energy (TKE) is also predicted for the PBL. The PBL-top mass entrainment is determined through an equation including the effects of TKE and the radiative and evaporative cooling processes concentrated near the PBL top. The surface fluxes are determined from an aerodynamic formula in which the velocity scale depends both on the square root of TKE and the grid-scale PBL velocity at the lowermost model layer. The turbulent fluxes within the PBL are determined through an approach that includes the effects of both large convective and small diffusive eddies. AGCM simulations with the new formulation of PBL are analyzed with a focus on the seasonal and diurnal variations. The simulated seasonal cycle of stratocumulus over the eastern oceans is realistic, as are the diurnal cycles of the PBL depth and precipitation over land. The simulated fluxes of latent heat, momentum, and shortwave radiation at the ocean surface and baroclinic activity in the middle latitudes show significant improvements over the previous versions of the AGCM based on the single-layer PBL.
    publisherAmerican Meteorological Society
    titleParameterization of PBL Processes in an Atmospheric General Circulation Model: Description and Preliminary Assessment
    typeJournal Paper
    journal volume137
    journal issue3
    journal titleMonthly Weather Review
    identifier doi10.1175/2008MWR2464.1
    journal fristpage1061
    journal lastpage1082
    treeMonthly Weather Review:;2009:;volume( 137 ):;issue: 003
    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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