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    Translation Effects on Simulated Tornadoes

    Source: Journal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 017::page 2574
    Author:
    Diamond, Chris J.
    ,
    Wilkins, Eugene M.
    DOI: 10.1175/1520-0469(1984)041<2574:TEOST>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A simulation of tornadoes translating over the ground was carried out in a modified Ward simulator. The purpose was to investigate the effects of translation on tornado dynamics. The results are as follows: ? Secondary vortexes were found to be generated by the relative motion between the main vortex and rough ?ground.? The secondary vortexes trail the primary vortex. Apparently they feed off the energy of the primary vortex, and achieve a momentary transition state from a single vortex to multiple vortexes. ? The core radius increases with swirl ratio and decreases with surface roughness. Translation causes a local increase in swirl ratio, increasing the core size over that of a stationary vortex. ? The central pressure drop increases with swirl ratio during translation. Translation also causes a steeper pressure gradient on the trailing side of the vortex core. A similar characteristic tilt on the trailing side of the pressure profile has been noted on barograms for real tornadoes.
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      Translation Effects on Simulated Tornadoes

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4154964
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    contributor authorDiamond, Chris J.
    contributor authorWilkins, Eugene M.
    date accessioned2017-06-09T14:25:10Z
    date available2017-06-09T14:25:10Z
    date copyright1984/09/01
    date issued1984
    identifier issn0022-4928
    identifier otherams-18907.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4154964
    description abstractA simulation of tornadoes translating over the ground was carried out in a modified Ward simulator. The purpose was to investigate the effects of translation on tornado dynamics. The results are as follows: ? Secondary vortexes were found to be generated by the relative motion between the main vortex and rough ?ground.? The secondary vortexes trail the primary vortex. Apparently they feed off the energy of the primary vortex, and achieve a momentary transition state from a single vortex to multiple vortexes. ? The core radius increases with swirl ratio and decreases with surface roughness. Translation causes a local increase in swirl ratio, increasing the core size over that of a stationary vortex. ? The central pressure drop increases with swirl ratio during translation. Translation also causes a steeper pressure gradient on the trailing side of the vortex core. A similar characteristic tilt on the trailing side of the pressure profile has been noted on barograms for real tornadoes.
    publisherAmerican Meteorological Society
    titleTranslation Effects on Simulated Tornadoes
    typeJournal Paper
    journal volume41
    journal issue17
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1984)041<2574:TEOST>2.0.CO;2
    journal fristpage2574
    journal lastpage2580
    treeJournal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 017
    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
    yabeshDSpacePersian