YaBeSH Engineering and Technology Library

    • Journals
    • PaperQuest
    • YSE Standards
    • YaBeSH
    • Login
    View Item 
    •   YE&T Library
    • AMS
    • Journal of the Atmospheric Sciences
    • View Item
    •   YE&T Library
    • AMS
    • Journal of the Atmospheric Sciences
    • View Item
    • All Fields
    • Source Title
    • Year
    • Publisher
    • Title
    • Subject
    • Author
    • DOI
    • ISBN
    Advanced Search
    JavaScript is disabled for your browser. Some features of this site may not work without it.

    Archive

    A Mean-Gradient Model of the Dry Convective Boundary Layer

    Source: Journal of the Atmospheric Sciences:;1989:;Volume( 047 ):;issue: 001::page 126
    Author:
    Wang, Shouping
    ,
    Albrecht, Bruce A.
    DOI: 10.1175/1520-0469(1990)047<0126:AMGMOT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A mean-gradient model of the dry convective boundary layer is developed using a convective mass flux representation of the turbulent fluxes. A top-hat model of thermals is used to represent the average characteristics of updrafts and downdrafts in the buoyantly driven circulation. The convective mass flux is related to the convective velocity scale. Although the model is computationally simple, it describes the basic structure of the CBL. In this parameterization the vertical gradients of conserved variables are controlled by internal mixing through vertical mass transports inside the convective boundary layer, bottom mixing due to the surface processes, top mixing due to the entrainment, and lateral mixing between updrafts and downdrafts.
    • Download: (929.5Kb)
    • Show Full MetaData Hide Full MetaData
    • Item Order
    • Go To Publisher
    • Price: 5000 Rial
    • Statistics

      A Mean-Gradient Model of the Dry Convective Boundary Layer

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4156461
    Collections
    • Journal of the Atmospheric Sciences

    Show full item record

    contributor authorWang, Shouping
    contributor authorAlbrecht, Bruce A.
    date accessioned2017-06-09T14:29:29Z
    date available2017-06-09T14:29:29Z
    date copyright1990/01/01
    date issued1989
    identifier issn0022-4928
    identifier otherams-20253.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4156461
    description abstractA mean-gradient model of the dry convective boundary layer is developed using a convective mass flux representation of the turbulent fluxes. A top-hat model of thermals is used to represent the average characteristics of updrafts and downdrafts in the buoyantly driven circulation. The convective mass flux is related to the convective velocity scale. Although the model is computationally simple, it describes the basic structure of the CBL. In this parameterization the vertical gradients of conserved variables are controlled by internal mixing through vertical mass transports inside the convective boundary layer, bottom mixing due to the surface processes, top mixing due to the entrainment, and lateral mixing between updrafts and downdrafts.
    publisherAmerican Meteorological Society
    titleA Mean-Gradient Model of the Dry Convective Boundary Layer
    typeJournal Paper
    journal volume47
    journal issue1
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1990)047<0126:AMGMOT>2.0.CO;2
    journal fristpage126
    journal lastpage138
    treeJournal of the Atmospheric Sciences:;1989:;Volume( 047 ):;issue: 001
    contenttypeFulltext
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian
     
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian