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    The Relationship between Tropopause Potential Temperature and the Buoyant Energy of Storm Air

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 020::page 2902
    Author:
    Chimonas, G.
    ,
    Rossi, R.
    DOI: 10.1175/1520-0469(1987)044<2902:TRBTPT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: It has been suggested that the potential temperature of the tropical tropopause may be linked to the energy of air flowing into storms, and Previous studies have sought to correlate the subannual fluctuations of the two quantities. The formulations used in these studies also provide estimates of the mean tropopause potential temperatures, but such temperatures are much lower than the observed values. In this work we reexamine the problem. The earlier thermodynamic formulation is replaced by a more accurate form, and the appropriate humidity content of storm air is introduced and justified. The data now show that, averaged over the tropical ocean regions, the mean potential temperature of the tropopause is determined accurately and directly by the mean sea surface temperature. Continental conditions are significantly different and require further study. It appears desirable to undertake detailed investigations of the local relationship between surface storm conditions and tropopause characteristics.
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      The Relationship between Tropopause Potential Temperature and the Buoyant Energy of Storm Air

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4155784
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    contributor authorChimonas, G.
    contributor authorRossi, R.
    date accessioned2017-06-09T14:27:41Z
    date available2017-06-09T14:27:41Z
    date copyright1987/10/01
    date issued1987
    identifier issn0022-4928
    identifier otherams-19645.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4155784
    description abstractIt has been suggested that the potential temperature of the tropical tropopause may be linked to the energy of air flowing into storms, and Previous studies have sought to correlate the subannual fluctuations of the two quantities. The formulations used in these studies also provide estimates of the mean tropopause potential temperatures, but such temperatures are much lower than the observed values. In this work we reexamine the problem. The earlier thermodynamic formulation is replaced by a more accurate form, and the appropriate humidity content of storm air is introduced and justified. The data now show that, averaged over the tropical ocean regions, the mean potential temperature of the tropopause is determined accurately and directly by the mean sea surface temperature. Continental conditions are significantly different and require further study. It appears desirable to undertake detailed investigations of the local relationship between surface storm conditions and tropopause characteristics.
    publisherAmerican Meteorological Society
    titleThe Relationship between Tropopause Potential Temperature and the Buoyant Energy of Storm Air
    typeJournal Paper
    journal volume44
    journal issue20
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1987)044<2902:TRBTPT>2.0.CO;2
    journal fristpage2902
    journal lastpage2911
    treeJournal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 020
    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