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    Details of Colliding Thunderstorm Outflows as Observed by Doppler Lidar

    Source: Journal of the Atmospheric Sciences:;1989:;Volume( 047 ):;issue: 009::page 1081
    Author:
    Intrieri, J. M.
    ,
    Bedard, A. J.
    ,
    Hardesty, R. M.
    DOI: 10.1175/1520-0469(1990)047<1081:DOCTOA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Three cases of colliding outflow boundaries are examined using data collected from the NOAA Doppler lidar and a meteorological tower during the summer of 1986 near Boulder, Colorado. The data are unique because the lidar and the 300 m tower were colocated, providing measurements of both kinematic and thermodynamic properties. Lidar data reveal small-scale vortex roll instabilities within the leading edge of the outflow. Observations of the post-collision interactions showed that the warmer of the two outflows was deflected upward by the colder outflow to heights of 2 km. In all cases, this forced mechanical lifting was sufficient to produce convection. A simple model of two colliding density currents also suggests that deeper outflows are more efficient in initiating convection.
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      Details of Colliding Thunderstorm Outflows as Observed by Doppler Lidar

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4156528
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    contributor authorIntrieri, J. M.
    contributor authorBedard, A. J.
    contributor authorHardesty, R. M.
    date accessioned2017-06-09T14:29:42Z
    date available2017-06-09T14:29:42Z
    date copyright1990/05/01
    date issued1989
    identifier issn0022-4928
    identifier otherams-20313.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4156528
    description abstractThree cases of colliding outflow boundaries are examined using data collected from the NOAA Doppler lidar and a meteorological tower during the summer of 1986 near Boulder, Colorado. The data are unique because the lidar and the 300 m tower were colocated, providing measurements of both kinematic and thermodynamic properties. Lidar data reveal small-scale vortex roll instabilities within the leading edge of the outflow. Observations of the post-collision interactions showed that the warmer of the two outflows was deflected upward by the colder outflow to heights of 2 km. In all cases, this forced mechanical lifting was sufficient to produce convection. A simple model of two colliding density currents also suggests that deeper outflows are more efficient in initiating convection.
    publisherAmerican Meteorological Society
    titleDetails of Colliding Thunderstorm Outflows as Observed by Doppler Lidar
    typeJournal Paper
    journal volume47
    journal issue9
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1990)047<1081:DOCTOA>2.0.CO;2
    journal fristpage1081
    journal lastpage1099
    treeJournal of the Atmospheric Sciences:;1989:;Volume( 047 ):;issue: 009
    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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