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    Piecewise Potential Vorticity Inversion and Vortex Interaction

    Source: Journal of the Atmospheric Sciences:;2009:;Volume( 066 ):;issue: 010::page 3208
    Author:
    Egger, Joseph
    DOI: 10.1175/2009JAS3079.1
    Publisher: American Meteorological Society
    Abstract: Piecewise potential vorticity inversion (PPVI) aims at an interpretation of the interaction of potential vorticity (PV) anomalies q. The total flow domain D is divided into subdomains D1 and D2 with q1 and q2 as PV anomalies. PPVI estimates the height tendency in D that results if q is transported by the winds obtained by an inversion of a PV field with q = q1 in D1 and q = 0 in D2. Tests compare the actual height tendency to that obtained via PPVI. This method is applied to the interaction of vortices in quasigeostrophic shallow water, a problem generally accepted as a paradigm for PPVI. Indeed, results are excellent for vortex pairs. Combinations of more vortices, including vortex clusters akin to Rossby waves, are also exposed to tests. The utility of PPVI tendencies depends strongly on the arrangement of the vortices in that case. Very good agreement is found as well as cases with quite low skill. The reasons for this scatter are discussed and a dynamic interpretation of PPVI is proposed.
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      Piecewise Potential Vorticity Inversion and Vortex Interaction

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4210049
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    contributor authorEgger, Joseph
    date accessioned2017-06-09T16:28:20Z
    date available2017-06-09T16:28:20Z
    date copyright2009/10/01
    date issued2009
    identifier issn0022-4928
    identifier otherams-68486.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4210049
    description abstractPiecewise potential vorticity inversion (PPVI) aims at an interpretation of the interaction of potential vorticity (PV) anomalies q. The total flow domain D is divided into subdomains D1 and D2 with q1 and q2 as PV anomalies. PPVI estimates the height tendency in D that results if q is transported by the winds obtained by an inversion of a PV field with q = q1 in D1 and q = 0 in D2. Tests compare the actual height tendency to that obtained via PPVI. This method is applied to the interaction of vortices in quasigeostrophic shallow water, a problem generally accepted as a paradigm for PPVI. Indeed, results are excellent for vortex pairs. Combinations of more vortices, including vortex clusters akin to Rossby waves, are also exposed to tests. The utility of PPVI tendencies depends strongly on the arrangement of the vortices in that case. Very good agreement is found as well as cases with quite low skill. The reasons for this scatter are discussed and a dynamic interpretation of PPVI is proposed.
    publisherAmerican Meteorological Society
    titlePiecewise Potential Vorticity Inversion and Vortex Interaction
    typeJournal Paper
    journal volume66
    journal issue10
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/2009JAS3079.1
    journal fristpage3208
    journal lastpage3216
    treeJournal of the Atmospheric Sciences:;2009:;Volume( 066 ):;issue: 010
    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