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    A Vacillation in Atmospheric Energy Parameters

    Source: Journal of the Atmospheric Sciences:;1976:;Volume( 033 ):;issue: 011::page 2079
    Author:
    McGuirk, James P.
    ,
    Reiter, Elmar R.
    DOI: 10.1175/1520-0469(1976)033<2079:AVIAEP>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A strong, persistent and significant oscillation of about 24-day periodicity is observed in hemispheric-scale energy parameters during the winter season. The characteristics of this cycle are defined using 9.5 years of daily NMC gridded height and temperature fields. Analysis of northward eddy heat flux strongly suggests that baroclinic processes are involved in this oscillation. The vacillation acts primarily on the planetary-wave scale and some of its synoptic characteristics are investigated. A decomposition of eddy available potential energy by zone wavenumber shows that the vacillation tends to favor different wavenumbers in different years. The concept of a vacillation in orientation of trough and ridge line tilt is not substantiated.
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      A Vacillation in Atmospheric Energy Parameters

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4153042
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    contributor authorMcGuirk, James P.
    contributor authorReiter, Elmar R.
    date accessioned2017-06-09T14:19:13Z
    date available2017-06-09T14:19:13Z
    date copyright1976/11/01
    date issued1976
    identifier issn0022-4928
    identifier otherams-17177.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4153042
    description abstractA strong, persistent and significant oscillation of about 24-day periodicity is observed in hemispheric-scale energy parameters during the winter season. The characteristics of this cycle are defined using 9.5 years of daily NMC gridded height and temperature fields. Analysis of northward eddy heat flux strongly suggests that baroclinic processes are involved in this oscillation. The vacillation acts primarily on the planetary-wave scale and some of its synoptic characteristics are investigated. A decomposition of eddy available potential energy by zone wavenumber shows that the vacillation tends to favor different wavenumbers in different years. The concept of a vacillation in orientation of trough and ridge line tilt is not substantiated.
    publisherAmerican Meteorological Society
    titleA Vacillation in Atmospheric Energy Parameters
    typeJournal Paper
    journal volume33
    journal issue11
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1976)033<2079:AVIAEP>2.0.CO;2
    journal fristpage2079
    journal lastpage2093
    treeJournal of the Atmospheric Sciences:;1976:;Volume( 033 ):;issue: 011
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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