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

    Cumulus Ensemble Effects on the Large-Scale Vorticity and Momentum Fields of GATE. Part II: Parameterization

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 046 ):;issue: 011::page 1609
    Author:
    Sui, Chung-Hsiung
    ,
    Cheng, Ming-Dean
    ,
    Wu, Xiaoqing
    ,
    Yanai, Michio
    DOI: 10.1175/1520-0469(1989)046<1609:CEEOTL>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A parameterization of cumulus ensemble effects on the large-scale vorticity is tested to interpret the vorticity budget residual, Z, observed during Phase III of GARP Atlantic Tropical Experiment (GATE). The parameterization is derived consistently from the parameterization of cumulus ensemble effects on the momentum equation. Values of the parameterized Z are computed using the cumulus properties (mass flux, mass detrainment and cloud momentum) diagnosed by a spectral cumulus ensemble model. The results confirm the inferences made in Part I of this paper that organized cumulus convection produces significant residuals in the large-scale vorticity budget mainly through 1) the detrainment of excess momentum from clouds, and 2) the vertical advection of the large-scale vorticity due to the subsidence of environmental air compensating the convective mass flux. In addition, the twisting of the horizontal component of the large-scale vorticity into the vertical component due to nonuniform spatial distributions of the convective mass flux plays a significant role in producing Z at the levels where the vertical wind shear is large. Deep cumulus convection decelerates the mean flow over the area of convection by the detrainment of smaller cloud momentum transported from below. This deceleration produces a positive vorticity tendency to the right of the convective area facing downstream and a negative tendency to the left. In addition, the curl of the excess momentum tends to produce a positive vorticity tendency over the area of convection. These effects explain the observed features of Z in the upper troposphere, i.e., the horizontal dipole pattern and the positive mean values. The vertical advection of the large-scale vorticity by the cumulus-induced subsidence is the dominant mechanism producing negative Z in the middle troposphere where the gradient of vorticity, ???/?p, is positive. In the lower troposphere where ???/?p is negative, the vertical advection effect produces positive Z. In addition, detrainment of momentum from shallow clouds is found to be significant near 650 mb and responsible for generating localized patterns in the horizontal distribution of Z. Results of additional experiments show improvements of the parameterized Z in the lower troposphere by including downdrafts in the diagnosis of mass flux and the potential importance of pressure interactions between the clouds and the environment in the cumulus momentum budget.
    • Download: (1.463Mb)
    • Show Full MetaData Hide Full MetaData
    • Item Order
    • Go To Publisher
    • Price: 5000 Rial
    • Statistics

      Cumulus Ensemble Effects on the Large-Scale Vorticity and Momentum Fields of GATE. Part II: Parameterization

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4156277
    Collections
    • Journal of the Atmospheric Sciences

    Show full item record

    contributor authorSui, Chung-Hsiung
    contributor authorCheng, Ming-Dean
    contributor authorWu, Xiaoqing
    contributor authorYanai, Michio
    date accessioned2017-06-09T14:29:00Z
    date available2017-06-09T14:29:00Z
    date copyright1989/06/01
    date issued1988
    identifier issn0022-4928
    identifier otherams-20088.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4156277
    description abstractA parameterization of cumulus ensemble effects on the large-scale vorticity is tested to interpret the vorticity budget residual, Z, observed during Phase III of GARP Atlantic Tropical Experiment (GATE). The parameterization is derived consistently from the parameterization of cumulus ensemble effects on the momentum equation. Values of the parameterized Z are computed using the cumulus properties (mass flux, mass detrainment and cloud momentum) diagnosed by a spectral cumulus ensemble model. The results confirm the inferences made in Part I of this paper that organized cumulus convection produces significant residuals in the large-scale vorticity budget mainly through 1) the detrainment of excess momentum from clouds, and 2) the vertical advection of the large-scale vorticity due to the subsidence of environmental air compensating the convective mass flux. In addition, the twisting of the horizontal component of the large-scale vorticity into the vertical component due to nonuniform spatial distributions of the convective mass flux plays a significant role in producing Z at the levels where the vertical wind shear is large. Deep cumulus convection decelerates the mean flow over the area of convection by the detrainment of smaller cloud momentum transported from below. This deceleration produces a positive vorticity tendency to the right of the convective area facing downstream and a negative tendency to the left. In addition, the curl of the excess momentum tends to produce a positive vorticity tendency over the area of convection. These effects explain the observed features of Z in the upper troposphere, i.e., the horizontal dipole pattern and the positive mean values. The vertical advection of the large-scale vorticity by the cumulus-induced subsidence is the dominant mechanism producing negative Z in the middle troposphere where the gradient of vorticity, ???/?p, is positive. In the lower troposphere where ???/?p is negative, the vertical advection effect produces positive Z. In addition, detrainment of momentum from shallow clouds is found to be significant near 650 mb and responsible for generating localized patterns in the horizontal distribution of Z. Results of additional experiments show improvements of the parameterized Z in the lower troposphere by including downdrafts in the diagnosis of mass flux and the potential importance of pressure interactions between the clouds and the environment in the cumulus momentum budget.
    publisherAmerican Meteorological Society
    titleCumulus Ensemble Effects on the Large-Scale Vorticity and Momentum Fields of GATE. Part II: Parameterization
    typeJournal Paper
    journal volume46
    journal issue11
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1989)046<1609:CEEOTL>2.0.CO;2
    journal fristpage1609
    journal lastpage1629
    treeJournal of the Atmospheric Sciences:;1988:;Volume( 046 ):;issue: 011
    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