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    TURBULENCE THEORY APPLIED TO LARGE-SCALE ATMOSPHERIC PHENOMENA

    Source: Journal of Meteorology:;1955:;volume( 012 ):;issue: 003::page 263
    Author:
    Hutchings, J. W.
    DOI: 10.1175/1520-0469(1955)012<0263:TTATLS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: An outline is given of a preliminary attempt to apply the methods which have proved serviceable in the treatment of small-scale turbulence to the wider problem of large-scale turbulence in the atmosphere. In particular, application is made of theoretical results giving the form of the correlation function for velocity fluctuations in the inertial range according to the theory of Kolmogoroff. It appears that some of these results may be valid over a considerably greater range of eddy sizes than might at first have been anticipated. Some attempt is also made to apply these methods to the determination of the cprrelation functions for larger-scale fluctuations of pressure and temperature in the atmosphere. Actual data taken at the earth's surface and in the free atmosphere are used to test the validity of these deductions.
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      TURBULENCE THEORY APPLIED TO LARGE-SCALE ATMOSPHERIC PHENOMENA

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4149699
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    contributor authorHutchings, J. W.
    date accessioned2017-06-09T14:11:14Z
    date available2017-06-09T14:11:14Z
    date copyright1955/06/01
    date issued1955
    identifier issn0095-9634
    identifier otherams-14168.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149699
    description abstractAn outline is given of a preliminary attempt to apply the methods which have proved serviceable in the treatment of small-scale turbulence to the wider problem of large-scale turbulence in the atmosphere. In particular, application is made of theoretical results giving the form of the correlation function for velocity fluctuations in the inertial range according to the theory of Kolmogoroff. It appears that some of these results may be valid over a considerably greater range of eddy sizes than might at first have been anticipated. Some attempt is also made to apply these methods to the determination of the cprrelation functions for larger-scale fluctuations of pressure and temperature in the atmosphere. Actual data taken at the earth's surface and in the free atmosphere are used to test the validity of these deductions.
    publisherAmerican Meteorological Society
    titleTURBULENCE THEORY APPLIED TO LARGE-SCALE ATMOSPHERIC PHENOMENA
    typeJournal Paper
    journal volume12
    journal issue3
    journal titleJournal of Meteorology
    identifier doi10.1175/1520-0469(1955)012<0263:TTATLS>2.0.CO;2
    journal fristpage263
    journal lastpage271
    treeJournal of Meteorology:;1955:;volume( 012 ):;issue: 003
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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