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    Entropy and Potential Temperature

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 020::page 2887
    Author:
    Hauf, Thomas
    ,
    Höller, Hartmut
    DOI: 10.1175/1520-0469(1987)044<2887:EAPT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The theoretical investigations presented in this paper show that the various definitions of potential temperatures, such as the potential temperature of dry air and of moist air, the equivalent potential temperature, the liquid water potential temperature, the ice-liquid water potential temperature and the wet equivalent potential temperature can be unified by one single definition. This general potential temperature is named the entropy temperature as it is a measure of entropy. The entropy state function for a system of cloudy air and the entropy budget are presented and discussed. For each of the potential temperatures the respective thermodynamic equation for which the potential temperature is an integral of the form, ? = constant, is reviewed on the basis of the entropy concept. As one result, it is found that the ice-liquid water potential temperature ?il is only an integral of the corresponding thermodynamic equation if saturation or chemical equilibrium between water vapor and liquid water or ice is assumed. A prognostic equation for the entropy temperature is derived using the entropy budget equation. This equation describes irreversible effects and holds also for an open system. From this equation exact prognostic equations for each of the potential temperatures can, at least in principle, be derived.
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      Entropy and Potential Temperature

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    contributor authorHauf, Thomas
    contributor authorHöller, Hartmut
    date accessioned2017-06-09T14:27:40Z
    date available2017-06-09T14:27:40Z
    date copyright1987/10/01
    date issued1987
    identifier issn0022-4928
    identifier otherams-19644.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4155783
    description abstractThe theoretical investigations presented in this paper show that the various definitions of potential temperatures, such as the potential temperature of dry air and of moist air, the equivalent potential temperature, the liquid water potential temperature, the ice-liquid water potential temperature and the wet equivalent potential temperature can be unified by one single definition. This general potential temperature is named the entropy temperature as it is a measure of entropy. The entropy state function for a system of cloudy air and the entropy budget are presented and discussed. For each of the potential temperatures the respective thermodynamic equation for which the potential temperature is an integral of the form, ? = constant, is reviewed on the basis of the entropy concept. As one result, it is found that the ice-liquid water potential temperature ?il is only an integral of the corresponding thermodynamic equation if saturation or chemical equilibrium between water vapor and liquid water or ice is assumed. A prognostic equation for the entropy temperature is derived using the entropy budget equation. This equation describes irreversible effects and holds also for an open system. From this equation exact prognostic equations for each of the potential temperatures can, at least in principle, be derived.
    publisherAmerican Meteorological Society
    titleEntropy and Potential Temperature
    typeJournal Paper
    journal volume44
    journal issue20
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1987)044<2887:EAPT>2.0.CO;2
    journal fristpage2887
    journal lastpage2901
    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
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