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    African Easterly Waves and Convection. Part I: Linear Simulations

    Source: Journal of the Atmospheric Sciences:;1995:;Volume( 052 ):;issue: 010::page 1657
    Author:
    Paradis, D.
    ,
    Lafore, J-P.
    ,
    Redelsperger, J-L.
    ,
    Balaji, V.
    DOI: 10.1175/1520-0469(1995)052<1657:AEWACP>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A linearized version of a nonhydrostatic model is used to study the normal-mode selection and the structure of the African easterly waves in dry and moist environments associated with an idealized African easterly jet structure. The dry mode reproduces the principal observed characteristics of the lower troposphere, in particular the low-level ascent and convergence in the trough. A simple CISK-type parameterization improves the upper-level circulation. A budget of kinetic energy shows barotropic and baroclinic contributions and adequately reproduces the analysis of Norquist et al. The scale selection and the structure of the most unstable mode appears sensitive to the jet structure, in particular to the meridional and vertical shear. Several discrepancies between observations and these linear modes emphasize the importance of an accurate description of convection.
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      African Easterly Waves and Convection. Part I: Linear Simulations

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4157807
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    contributor authorParadis, D.
    contributor authorLafore, J-P.
    contributor authorRedelsperger, J-L.
    contributor authorBalaji, V.
    date accessioned2017-06-09T14:33:02Z
    date available2017-06-09T14:33:02Z
    date copyright1995/05/01
    date issued1995
    identifier issn0022-4928
    identifier otherams-21465.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4157807
    description abstractA linearized version of a nonhydrostatic model is used to study the normal-mode selection and the structure of the African easterly waves in dry and moist environments associated with an idealized African easterly jet structure. The dry mode reproduces the principal observed characteristics of the lower troposphere, in particular the low-level ascent and convergence in the trough. A simple CISK-type parameterization improves the upper-level circulation. A budget of kinetic energy shows barotropic and baroclinic contributions and adequately reproduces the analysis of Norquist et al. The scale selection and the structure of the most unstable mode appears sensitive to the jet structure, in particular to the meridional and vertical shear. Several discrepancies between observations and these linear modes emphasize the importance of an accurate description of convection.
    publisherAmerican Meteorological Society
    titleAfrican Easterly Waves and Convection. Part I: Linear Simulations
    typeJournal Paper
    journal volume52
    journal issue10
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1995)052<1657:AEWACP>2.0.CO;2
    journal fristpage1657
    journal lastpage1679
    treeJournal of the Atmospheric Sciences:;1995:;Volume( 052 ):;issue: 010
    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