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    The Observed Annual Cycle in the Meridional Transport of Atmospheric Energy

    Source: Journal of the Atmospheric Sciences:;1971:;Volume( 028 ):;issue: 003::page 325
    Author:
    Oort, Abraham H.
    DOI: 10.1175/1520-0469(1971)028<0325:TOACIT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The annual cycles in the atmospheric storage and in the meridional transport of energy are discussed. The calculations are based on a five-year sample from more than 500 radiosonde stations mainly located in the Northern Hemisphere. All statistics represent values integrated vertically between the earth's surface and 75 mb and horizontally along a latitude circle. Several new and interesting features of the eddy and mean transports of potential energy, sensible heat, latent heat and kinetic energy become apparent by the breakdown according to calendar month. In December through February more than half of the sensible heat is transported poleward by the standing eddies. The transient eddy heat flux does not peak in winter but in April and November. The strong annual cycle in the tropical Hadley circulation does not contribute to the poleward transfer of energy for the year as a whole.
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      The Observed Annual Cycle in the Meridional Transport of Atmospheric Energy

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    contributor authorOort, Abraham H.
    date accessioned2017-06-09T14:15:47Z
    date available2017-06-09T14:15:47Z
    date copyright1971/04/01
    date issued1971
    identifier issn0022-4928
    identifier otherams-15939.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4151666
    description abstractThe annual cycles in the atmospheric storage and in the meridional transport of energy are discussed. The calculations are based on a five-year sample from more than 500 radiosonde stations mainly located in the Northern Hemisphere. All statistics represent values integrated vertically between the earth's surface and 75 mb and horizontally along a latitude circle. Several new and interesting features of the eddy and mean transports of potential energy, sensible heat, latent heat and kinetic energy become apparent by the breakdown according to calendar month. In December through February more than half of the sensible heat is transported poleward by the standing eddies. The transient eddy heat flux does not peak in winter but in April and November. The strong annual cycle in the tropical Hadley circulation does not contribute to the poleward transfer of energy for the year as a whole.
    publisherAmerican Meteorological Society
    titleThe Observed Annual Cycle in the Meridional Transport of Atmospheric Energy
    typeJournal Paper
    journal volume28
    journal issue3
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1971)028<0325:TOACIT>2.0.CO;2
    journal fristpage325
    journal lastpage339
    treeJournal of the Atmospheric Sciences:;1971:;Volume( 028 ):;issue: 003
    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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