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    Nonlinear Effects on Convectively Forced Two-Dimensional Mesoscale Flows

    Source: Journal of the Atmospheric Sciences:;2012:;Volume( 069 ):;issue: 011::page 3391
    Author:
    Han, Ji-Young
    ,
    Baik, Jong-Jin
    DOI: 10.1175/JAS-D-11-0335.1
    Publisher: American Meteorological Society
    Abstract: ne of the important problems in mesoscale atmospheric dynamics is how the atmosphere responds to convective heating or cooling. Here, the authors examine nonlinear effects on convectively forced mesoscale flows in the context of the nonlinear response of a stably stratified flow to elevated steady heating in two dimensions using a nondimensional numerical model. Results of two-dimensional numerical experiments in a uniform flow show that even without vertical wind shear, a separation of an upwind cellular updraft from the steady heating-induced main updraft occurs in a highly nonlinear flow system. This separation occurs as the compensating cellular downdraft associated with a secondary maximum in the main updraft develops. As the nonlinearity of the flow system increases, the upwind cellular updraft is separated earlier and becomes stronger. Smaller viscous terms result in the separation of more cellular updrafts, which become stronger and move farther away from the main updraft region. In particular, in an inviscid flow, cellular updrafts are periodically separated from the main updraft, and the first cellular updraft and downdraft have intensities comparable to the intensity of the main updraft. In a viscid flow with a constant vertical wind shear up to a certain height, the propagating cellular updraft and downdraft are produced when the nonlinearity is large, as in a uniform flow. Stronger vertical wind shear leads to the earlier formation of the cellular updraft and its stronger intensity, faster propagating speed, and longer lifetime. Results of numerical experiments with squall line?type forcing imply that the highly nonlinear state is necessary for the development of cellular updrafts.
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      Nonlinear Effects on Convectively Forced Two-Dimensional Mesoscale Flows

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4218869
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    contributor authorHan, Ji-Young
    contributor authorBaik, Jong-Jin
    date accessioned2017-06-09T16:54:54Z
    date available2017-06-09T16:54:54Z
    date copyright2012/11/01
    date issued2012
    identifier issn0022-4928
    identifier otherams-76423.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4218869
    description abstractne of the important problems in mesoscale atmospheric dynamics is how the atmosphere responds to convective heating or cooling. Here, the authors examine nonlinear effects on convectively forced mesoscale flows in the context of the nonlinear response of a stably stratified flow to elevated steady heating in two dimensions using a nondimensional numerical model. Results of two-dimensional numerical experiments in a uniform flow show that even without vertical wind shear, a separation of an upwind cellular updraft from the steady heating-induced main updraft occurs in a highly nonlinear flow system. This separation occurs as the compensating cellular downdraft associated with a secondary maximum in the main updraft develops. As the nonlinearity of the flow system increases, the upwind cellular updraft is separated earlier and becomes stronger. Smaller viscous terms result in the separation of more cellular updrafts, which become stronger and move farther away from the main updraft region. In particular, in an inviscid flow, cellular updrafts are periodically separated from the main updraft, and the first cellular updraft and downdraft have intensities comparable to the intensity of the main updraft. In a viscid flow with a constant vertical wind shear up to a certain height, the propagating cellular updraft and downdraft are produced when the nonlinearity is large, as in a uniform flow. Stronger vertical wind shear leads to the earlier formation of the cellular updraft and its stronger intensity, faster propagating speed, and longer lifetime. Results of numerical experiments with squall line?type forcing imply that the highly nonlinear state is necessary for the development of cellular updrafts.
    publisherAmerican Meteorological Society
    titleNonlinear Effects on Convectively Forced Two-Dimensional Mesoscale Flows
    typeJournal Paper
    journal volume69
    journal issue11
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/JAS-D-11-0335.1
    journal fristpage3391
    journal lastpage3404
    treeJournal of the Atmospheric Sciences:;2012:;Volume( 069 ):;issue: 011
    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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