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    THE SPECTRA OF LARGE-SCALE TURBULENT TRANSFER OF MOMENTUM AND HEAT

    Source: Journal of Meteorology:;1960:;volume( 017 ):;issue: 004::page 435
    Author:
    Chiu, Wan-cheng
    DOI: 10.1175/1520-0469(1960)017<0435:TSOLST>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The spectra of large-scale eddy transfer of angular momentum and heat were constructed for seven levels, ranging from 700 mb to 50 mb over Belmar, N. J., and at the 300-mb and 200-mb levels over Cocoa, Florida. It is found that the frequencies of motion which were largely responsible for the eddy transport of heat shift toward lower frequencies with height. There was no such frequency shift indicated in the case of momentum transfer. The spectral intensity for the transport of angular momentum, when plotted against frequency, in general decreases with increasing frequency. The disturbances of long periods (say, longer than 20 days) were found to play a role as important as those of shorter periods in contributing to the total eddy transport of both heat and momentum.
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      THE SPECTRA OF LARGE-SCALE TURBULENT TRANSFER OF MOMENTUM AND HEAT

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4150228
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    contributor authorChiu, Wan-cheng
    date accessioned2017-06-09T14:12:24Z
    date available2017-06-09T14:12:24Z
    date copyright1960/08/01
    date issued1960
    identifier issn0095-9634
    identifier otherams-14644.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150228
    description abstractThe spectra of large-scale eddy transfer of angular momentum and heat were constructed for seven levels, ranging from 700 mb to 50 mb over Belmar, N. J., and at the 300-mb and 200-mb levels over Cocoa, Florida. It is found that the frequencies of motion which were largely responsible for the eddy transport of heat shift toward lower frequencies with height. There was no such frequency shift indicated in the case of momentum transfer. The spectral intensity for the transport of angular momentum, when plotted against frequency, in general decreases with increasing frequency. The disturbances of long periods (say, longer than 20 days) were found to play a role as important as those of shorter periods in contributing to the total eddy transport of both heat and momentum.
    publisherAmerican Meteorological Society
    titleTHE SPECTRA OF LARGE-SCALE TURBULENT TRANSFER OF MOMENTUM AND HEAT
    typeJournal Paper
    journal volume17
    journal issue4
    journal titleJournal of Meteorology
    identifier doi10.1175/1520-0469(1960)017<0435:TSOLST>2.0.CO;2
    journal fristpage435
    journal lastpage441
    treeJournal of Meteorology:;1960:;volume( 017 ):;issue: 004
    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