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    Three-dimensional Scaling and Structure of Atmospheric Energetics

    Source: Journal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 001::page 52
    Author:
    Baer, Ferdinand
    DOI: 10.1175/1520-0469(1981)038<0052:TDSASO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Three-dimensional structure functions characteristic of atmospheric energy are developed from data samples and presented. The horizontal dependence is based on known functions in spherical surfaces whereas the vertical dependence is derived from data. Three-dimensional scaling of these functions is determined from the properties of the functions as well as their ability to satisfy the potential vorticity equation. The distribution of observed planetary energy represented by these functions is presented in terms of their scale. Two-dimensional energy distributions in each of the vertical modes are also described. Power law relationships of energy versus scale with slope of ?3 appear in the statistics, but not under all conditions. The results of the study may be useful in parameterizing non-resolved model scales for closure. The structure functions may be utilized for fully three-dimensional spectral modeling. The scaling of the structure functions indicates appropriate vertical resolution for given horizontal model truncation as well as the appropriate vertical levels to be selected.
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      Three-dimensional Scaling and Structure of Atmospheric Energetics

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    contributor authorBaer, Ferdinand
    date accessioned2017-06-09T14:22:02Z
    date available2017-06-09T14:22:02Z
    date copyright1981/01/01
    date issued1981
    identifier issn0022-4928
    identifier otherams-18061.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4154025
    description abstractThree-dimensional structure functions characteristic of atmospheric energy are developed from data samples and presented. The horizontal dependence is based on known functions in spherical surfaces whereas the vertical dependence is derived from data. Three-dimensional scaling of these functions is determined from the properties of the functions as well as their ability to satisfy the potential vorticity equation. The distribution of observed planetary energy represented by these functions is presented in terms of their scale. Two-dimensional energy distributions in each of the vertical modes are also described. Power law relationships of energy versus scale with slope of ?3 appear in the statistics, but not under all conditions. The results of the study may be useful in parameterizing non-resolved model scales for closure. The structure functions may be utilized for fully three-dimensional spectral modeling. The scaling of the structure functions indicates appropriate vertical resolution for given horizontal model truncation as well as the appropriate vertical levels to be selected.
    publisherAmerican Meteorological Society
    titleThree-dimensional Scaling and Structure of Atmospheric Energetics
    typeJournal Paper
    journal volume38
    journal issue1
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1981)038<0052:TDSASO>2.0.CO;2
    journal fristpage52
    journal lastpage68
    treeJournal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 001
    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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