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    The Partitioning of the Poleward Energy Transport between the Tropical Ocean and Atmosphere

    Source: Journal of the Atmospheric Sciences:;2001:;Volume( 058 ):;issue: 008::page 943
    Author:
    Held, Isaac M.
    DOI: 10.1175/1520-0469(2001)058<0943:TPOTPE>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The mass transport in the shallow, wind-driven, overturning cells in the tropical oceans is constrained to be close to the mass transport in the atmospheric Hadley cell, assuming that zonally integrated wind stresses on land are relatively small. Therefore, the ratio of the poleward energy transport in low latitudes in the two media is determined by the ratio of the atmospheric gross static stability to that of the ocean. A qualitative discussion of the gross stability of each medium suggests that the resulting ratio of oceanic to atmospheric energy transport, averaged over the Hadley cell, is roughly equal to the ratio of the heat capacity of water to that of air at constant pressure, multiplied by the ratio of the moist- to the dry-adiabatic lapse rates near the surface. The ratio of oceanic to atmospheric energy transport should be larger than this value near the equator and smaller than this value near the poleward boundary of the Hadley cell.
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      The Partitioning of the Poleward Energy Transport between the Tropical Ocean and Atmosphere

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    contributor authorHeld, Isaac M.
    date accessioned2017-06-09T14:36:48Z
    date available2017-06-09T14:36:48Z
    date copyright2001/04/01
    date issued2001
    identifier issn0022-4928
    identifier otherams-22817.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4159309
    description abstractThe mass transport in the shallow, wind-driven, overturning cells in the tropical oceans is constrained to be close to the mass transport in the atmospheric Hadley cell, assuming that zonally integrated wind stresses on land are relatively small. Therefore, the ratio of the poleward energy transport in low latitudes in the two media is determined by the ratio of the atmospheric gross static stability to that of the ocean. A qualitative discussion of the gross stability of each medium suggests that the resulting ratio of oceanic to atmospheric energy transport, averaged over the Hadley cell, is roughly equal to the ratio of the heat capacity of water to that of air at constant pressure, multiplied by the ratio of the moist- to the dry-adiabatic lapse rates near the surface. The ratio of oceanic to atmospheric energy transport should be larger than this value near the equator and smaller than this value near the poleward boundary of the Hadley cell.
    publisherAmerican Meteorological Society
    titleThe Partitioning of the Poleward Energy Transport between the Tropical Ocean and Atmosphere
    typeJournal Paper
    journal volume58
    journal issue8
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(2001)058<0943:TPOTPE>2.0.CO;2
    journal fristpage943
    journal lastpage948
    treeJournal of the Atmospheric Sciences:;2001:;Volume( 058 ):;issue: 008
    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