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    The Meandering Nature of Tropical Cyclone Tracks

    Source: Journal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 009::page 1254
    Author:
    Holland, Greg J.
    ,
    Lander, Mark
    DOI: 10.1175/1520-0469(1993)050<1254:TMNOTC>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The observed tendency for tropical cyclones to meander about a longer-term track with periods of several days and amplitudes around 100 km is investigated. An analysis of 26 cyclones in the western North Pacific Ocean does not support the theories by Syono and Futi that tropical cyclone track oscillations occur from excitation of inertial oscillations. The observations and related numerical modeling studies also do not support the vortex patch and rotating cylinder theories by Yeh and Kuo. It is suggested that many meanders occur from interactions with mesoscale vortices and convective systems within the cyclone circulation. This hypothesis is supported by a case study of the effects of mesoscale convective complexes that developed in Typhoon Sarah (1989).
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      The Meandering Nature of Tropical Cyclone Tracks

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4157185
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    contributor authorHolland, Greg J.
    contributor authorLander, Mark
    date accessioned2017-06-09T14:31:25Z
    date available2017-06-09T14:31:25Z
    date copyright1993/05/01
    date issued1993
    identifier issn0022-4928
    identifier otherams-20905.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4157185
    description abstractThe observed tendency for tropical cyclones to meander about a longer-term track with periods of several days and amplitudes around 100 km is investigated. An analysis of 26 cyclones in the western North Pacific Ocean does not support the theories by Syono and Futi that tropical cyclone track oscillations occur from excitation of inertial oscillations. The observations and related numerical modeling studies also do not support the vortex patch and rotating cylinder theories by Yeh and Kuo. It is suggested that many meanders occur from interactions with mesoscale vortices and convective systems within the cyclone circulation. This hypothesis is supported by a case study of the effects of mesoscale convective complexes that developed in Typhoon Sarah (1989).
    publisherAmerican Meteorological Society
    titleThe Meandering Nature of Tropical Cyclone Tracks
    typeJournal Paper
    journal volume50
    journal issue9
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1993)050<1254:TMNOTC>2.0.CO;2
    journal fristpage1254
    journal lastpage1266
    treeJournal of the Atmospheric Sciences:;1993:;Volume( 050 ):;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
    yabeshDSpacePersian