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    The Frontogenetical Forcing of Secondary Circulations. Part I: The Duality and Generalization of the Q Vector

    Source: Journal of the Atmospheric Sciences:;1991:;Volume( 048 ):;issue: 004::page 497
    Author:
    Davies-Jones, Robert
    DOI: 10.1175/1520-0469(1991)048<0497:TFFOSC>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Hoskins, Draghici, and others have shown that the Q vector is an important quantity in quasi-geostrophic (QG) theory for the diagnosis of ageostrophic circulations. In this paper, a vorticity dynamics perspective is used to develop a generalized Q vector, Q*. An equation that relates the material derivative of the thermal-wind imbalance vector to Q* and ageostrophic terms in isentropic flow is obtained from the primitive equations (PE). The generalized Q vector is the vector mean of two terms: a frontogenetical vector that, for horizontal isentropic flow, is equal to the vector frontogenesis function F, and a vortex stretching term proportional to the stretching and reorientation of vorticity by the horizontal wind. Invoking just one QG assumption, the substitution of geostrophic for total velocity gradients, reduces Q* to Q and leads directly to the omega equation of QG theory. The frontogenetical and vortex stretching parts of the generalized Q vector of PE theory become equal in the QG limit. Thus, the conventional Q vector has dual physical interpretations in terms of vorticity and thermodynamic properties. The divergence of the Q vector in its vortex stretching form is equal to the forcing term in the Sutcliffe, Wiin-Nielsen, and Trenberth version of the omega equation. The self-destruction of balanced flow and its restoration by vertical secondary circulations is explained in terms of entropy and vorticity properties. A new assumption (Alternative Balance or AB) consists of omitting the material derivative of the thermal-wind imbalance vector, so that thermal-wind balance is restored instantaneously by secondary circulations. This approximation reduces the PE omega and secondary circulation equations to diagnostic forms resembling their QG equivalents, except for the replacement of Q by Q*. Under the AB assumption, the Q* vector points toward rising motion and inertial gravity waves are excluded.
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      The Frontogenetical Forcing of Secondary Circulations. Part I: The Duality and Generalization of the Q Vector

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    contributor authorDavies-Jones, Robert
    date accessioned2017-06-09T14:30:10Z
    date available2017-06-09T14:30:10Z
    date copyright1991/02/01
    date issued1991
    identifier issn0022-4928
    identifier otherams-20483.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4156716
    description abstractHoskins, Draghici, and others have shown that the Q vector is an important quantity in quasi-geostrophic (QG) theory for the diagnosis of ageostrophic circulations. In this paper, a vorticity dynamics perspective is used to develop a generalized Q vector, Q*. An equation that relates the material derivative of the thermal-wind imbalance vector to Q* and ageostrophic terms in isentropic flow is obtained from the primitive equations (PE). The generalized Q vector is the vector mean of two terms: a frontogenetical vector that, for horizontal isentropic flow, is equal to the vector frontogenesis function F, and a vortex stretching term proportional to the stretching and reorientation of vorticity by the horizontal wind. Invoking just one QG assumption, the substitution of geostrophic for total velocity gradients, reduces Q* to Q and leads directly to the omega equation of QG theory. The frontogenetical and vortex stretching parts of the generalized Q vector of PE theory become equal in the QG limit. Thus, the conventional Q vector has dual physical interpretations in terms of vorticity and thermodynamic properties. The divergence of the Q vector in its vortex stretching form is equal to the forcing term in the Sutcliffe, Wiin-Nielsen, and Trenberth version of the omega equation. The self-destruction of balanced flow and its restoration by vertical secondary circulations is explained in terms of entropy and vorticity properties. A new assumption (Alternative Balance or AB) consists of omitting the material derivative of the thermal-wind imbalance vector, so that thermal-wind balance is restored instantaneously by secondary circulations. This approximation reduces the PE omega and secondary circulation equations to diagnostic forms resembling their QG equivalents, except for the replacement of Q by Q*. Under the AB assumption, the Q* vector points toward rising motion and inertial gravity waves are excluded.
    publisherAmerican Meteorological Society
    titleThe Frontogenetical Forcing of Secondary Circulations. Part I: The Duality and Generalization of the Q Vector
    typeJournal Paper
    journal volume48
    journal issue4
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1991)048<0497:TFFOSC>2.0.CO;2
    journal fristpage497
    journal lastpage509
    treeJournal of the Atmospheric Sciences:;1991:;Volume( 048 ):;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
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