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    THE INCREASE OR DECREASE OF MEAN-FLOW ENERGY IN LARGE-SCALE HORIZONTAL FLOW IN THE ATMOSPHERE

    Source: Journal of Meteorology:;1952:;volume( 009 ):;issue: 005::page 347
    Author:
    Platzman, George W.
    DOI: 10.1175/1520-0469(1952)009<0347:TIODOM>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The transfer of energy between mean flow and disturbance for a barotropic non-divergent fluid is investigated by solution of the vorticity equation to obtain initial tendencies corresponding to assigned flow-patterns. The initial rate and direction of energy transfer are computed for different types of mean flow and disturbance. These calculations suggest that the form, as well as the wavelength, of the disturbance is a controlling factor in determining the initial energy-transfer, and that conclusive inferences cannot be made merely from the character of the mean flow. The distribution of initial changes in mean flow is calculated in several cases; it is found that, for both initially amplified and initially damped disturbances, momentum may be transferred from both sides into a central zone of maximum mean flow.
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      THE INCREASE OR DECREASE OF MEAN-FLOW ENERGY IN LARGE-SCALE HORIZONTAL FLOW IN THE ATMOSPHERE

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4149433
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    contributor authorPlatzman, George W.
    date accessioned2017-06-09T14:10:37Z
    date available2017-06-09T14:10:37Z
    date copyright1952/10/01
    date issued1952
    identifier issn0095-9634
    identifier otherams-13929.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149433
    description abstractThe transfer of energy between mean flow and disturbance for a barotropic non-divergent fluid is investigated by solution of the vorticity equation to obtain initial tendencies corresponding to assigned flow-patterns. The initial rate and direction of energy transfer are computed for different types of mean flow and disturbance. These calculations suggest that the form, as well as the wavelength, of the disturbance is a controlling factor in determining the initial energy-transfer, and that conclusive inferences cannot be made merely from the character of the mean flow. The distribution of initial changes in mean flow is calculated in several cases; it is found that, for both initially amplified and initially damped disturbances, momentum may be transferred from both sides into a central zone of maximum mean flow.
    publisherAmerican Meteorological Society
    titleTHE INCREASE OR DECREASE OF MEAN-FLOW ENERGY IN LARGE-SCALE HORIZONTAL FLOW IN THE ATMOSPHERE
    typeJournal Paper
    journal volume9
    journal issue5
    journal titleJournal of Meteorology
    identifier doi10.1175/1520-0469(1952)009<0347:TIODOM>2.0.CO;2
    journal fristpage347
    journal lastpage358
    treeJournal of Meteorology:;1952:;volume( 009 ):;issue: 005
    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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