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    ON THE LOW-LEVEL STRUCTURE OF TROPICAL STORMS

    Source: Journal of Meteorology:;1952:;volume( 009 ):;issue: 006::page 422
    Author:
    Hughes, Lawrence A.
    DOI: 10.1175/1520-0469(1952)009<0422:OTLLSO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Data from a number of reconnaissance flights into large Pacific tropical cyclones are combined to obtain a generalized pattern of winds at low level (about 1000 feet) under both stationary and non-stationary conditions. With these winds, a number of dependent computations are made including relative trajectories, divergence, vertical motion, rainfall, energy, and relative vorticity.
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      ON THE LOW-LEVEL STRUCTURE OF TROPICAL STORMS

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4149451
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    contributor authorHughes, Lawrence A.
    date accessioned2017-06-09T14:10:39Z
    date available2017-06-09T14:10:39Z
    date copyright1952/12/01
    date issued1952
    identifier issn0095-9634
    identifier otherams-13945.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149451
    description abstractData from a number of reconnaissance flights into large Pacific tropical cyclones are combined to obtain a generalized pattern of winds at low level (about 1000 feet) under both stationary and non-stationary conditions. With these winds, a number of dependent computations are made including relative trajectories, divergence, vertical motion, rainfall, energy, and relative vorticity.
    publisherAmerican Meteorological Society
    titleON THE LOW-LEVEL STRUCTURE OF TROPICAL STORMS
    typeJournal Paper
    journal volume9
    journal issue6
    journal titleJournal of Meteorology
    identifier doi10.1175/1520-0469(1952)009<0422:OTLLSO>2.0.CO;2
    journal fristpage422
    journal lastpage428
    treeJournal of Meteorology:;1952:;volume( 009 ):;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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