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    Frictional Dissipation in a Precipitating Atmosphere

    Source: Journal of the Atmospheric Sciences:;2000:;Volume( 057 ):;issue: 007::page 989
    Author:
    Pauluis, Olivier
    ,
    Balaji, V.
    ,
    Held, Isaac M.
    DOI: 10.1175/1520-0469(2000)057<0989:FDIAPA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The frictional dissipation in the shear zone surrounding falling hydrometeors is estimated to be 2?4 W m?2 in the Tropics. A numerical model of radiative?convective equilibrium with resolved three-dimensional moist convection confirms this estimate and shows that the precipitation-related dissipation is much larger than the dissipation associated with the turbulent energy cascade from the convective scale. Equivalently, the work performed by moist convection is used primarily to lift water rather than generate kinetic energy of the convective airflow. This fact complicates attempts to use the entropy budget to derive convective velocity scales.
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      Frictional Dissipation in a Precipitating Atmosphere

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    contributor authorPauluis, Olivier
    contributor authorBalaji, V.
    contributor authorHeld, Isaac M.
    date accessioned2017-06-09T14:36:03Z
    date available2017-06-09T14:36:03Z
    date copyright2000/04/01
    date issued2000
    identifier issn0022-4928
    identifier otherams-22569.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4159033
    description abstractThe frictional dissipation in the shear zone surrounding falling hydrometeors is estimated to be 2?4 W m?2 in the Tropics. A numerical model of radiative?convective equilibrium with resolved three-dimensional moist convection confirms this estimate and shows that the precipitation-related dissipation is much larger than the dissipation associated with the turbulent energy cascade from the convective scale. Equivalently, the work performed by moist convection is used primarily to lift water rather than generate kinetic energy of the convective airflow. This fact complicates attempts to use the entropy budget to derive convective velocity scales.
    publisherAmerican Meteorological Society
    titleFrictional Dissipation in a Precipitating Atmosphere
    typeJournal Paper
    journal volume57
    journal issue7
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(2000)057<0989:FDIAPA>2.0.CO;2
    journal fristpage989
    journal lastpage994
    treeJournal of the Atmospheric Sciences:;2000:;Volume( 057 ):;issue: 007
    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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