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    Microburst Rotation: Simulations and Observations

    Source: Journal of Applied Meteorology:;1995:;volume( 034 ):;issue: 006::page 1267
    Author:
    Rinehart, Ronald E.
    ,
    Borho, Alan
    ,
    Curtiss, Charles
    DOI: 10.1175/1520-0450(1995)034<1267:MRSAO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Microburst rotation can be determined by measuring the difference in azimuths between the maximum approaching and maximum receding velocity centers on a Doppler radar. Nonrotating microbursts would have these centers exactly along the same radial from the radar. Microbursts rotating clockwise would have the approaching center clockwise of the receding center, and vise versa. In the fist part of this study the authors develop the relationships between the uniform wind, source strength, and rotational strength using potential flow theory and apply this to simulating real microbursts. In the second part the authors give observations of microburst rotation based on measurements of 908 microbursts made near Orlando, Florida, during 1992. While most microbursts had little rotation, 55.4% rotated cyclonically. The average tangential velocity of the rotational component was 1.1 m s?1; 5% had rotations equal to or greater than 2.5 m s?1. This may have significant implications for aviation. Finally, microburst strength measurements are compared with velocity shear and F factors for the 908 microbursts.
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      Microburst Rotation: Simulations and Observations

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4147458
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    contributor authorRinehart, Ronald E.
    contributor authorBorho, Alan
    contributor authorCurtiss, Charles
    date accessioned2017-06-09T14:05:13Z
    date available2017-06-09T14:05:13Z
    date copyright1995/06/01
    date issued1995
    identifier issn0894-8763
    identifier otherams-12150.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4147458
    description abstractMicroburst rotation can be determined by measuring the difference in azimuths between the maximum approaching and maximum receding velocity centers on a Doppler radar. Nonrotating microbursts would have these centers exactly along the same radial from the radar. Microbursts rotating clockwise would have the approaching center clockwise of the receding center, and vise versa. In the fist part of this study the authors develop the relationships between the uniform wind, source strength, and rotational strength using potential flow theory and apply this to simulating real microbursts. In the second part the authors give observations of microburst rotation based on measurements of 908 microbursts made near Orlando, Florida, during 1992. While most microbursts had little rotation, 55.4% rotated cyclonically. The average tangential velocity of the rotational component was 1.1 m s?1; 5% had rotations equal to or greater than 2.5 m s?1. This may have significant implications for aviation. Finally, microburst strength measurements are compared with velocity shear and F factors for the 908 microbursts.
    publisherAmerican Meteorological Society
    titleMicroburst Rotation: Simulations and Observations
    typeJournal Paper
    journal volume34
    journal issue6
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1995)034<1267:MRSAO>2.0.CO;2
    journal fristpage1267
    journal lastpage1285
    treeJournal of Applied Meteorology:;1995:;volume( 034 ):;issue: 006
    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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