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    Vortex-Driven Sensitivity in Deformation Flow

    Source: Journal of the Atmospheric Sciences:;2008:;Volume( 065 ):;issue: 012::page 3819
    Author:
    Liu, Zhiyuan
    ,
    Roebber, Paul J.
    DOI: 10.1175/2008JAS2745.1
    Publisher: American Meteorological Society
    Abstract: A sensitivity mechanism for the interaction of two vortices in a two-dimensional deformation background flow is explored. A nonlinear model describing the vortex interaction up to a critical merging distance is developed. This model shows that in a confluent or diffluent background flow, two vortices can obtain a global minimum distance by counterclockwise turning and a local minimum distance by clockwise turning about each other. In a major portion of the phase space, the global minimum distance is smaller than the local minimum distance. Therefore, vortex merger is more likely to occur during the process in which the two vortices approach their global smallest distance. Analysis of the governing equations shows that there exists a ?most sensitive line? of initial vortex positions. When an initial state is on one side of the most sensitive line, the two vortices can obtain their global smallest distance and thus have a higher chance for merger. Conversely, when an initial state is on the other side relative to the most sensitive line, the two vortices can only obtain their local smallest distance. Consequently, they have a lower chance for merger. When an initial state is close to the most sensitive line, a very small initialization error can put this initial state on the wrong side of the most sensitive line, and the forecast evolution of the pair of vortices may be very different from the observed evolution. Numerical simulations that support these theoretical results are shown.
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      Vortex-Driven Sensitivity in Deformation Flow

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4208228
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    contributor authorLiu, Zhiyuan
    contributor authorRoebber, Paul J.
    date accessioned2017-06-09T16:22:56Z
    date available2017-06-09T16:22:56Z
    date copyright2008/12/01
    date issued2008
    identifier issn0022-4928
    identifier otherams-66847.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4208228
    description abstractA sensitivity mechanism for the interaction of two vortices in a two-dimensional deformation background flow is explored. A nonlinear model describing the vortex interaction up to a critical merging distance is developed. This model shows that in a confluent or diffluent background flow, two vortices can obtain a global minimum distance by counterclockwise turning and a local minimum distance by clockwise turning about each other. In a major portion of the phase space, the global minimum distance is smaller than the local minimum distance. Therefore, vortex merger is more likely to occur during the process in which the two vortices approach their global smallest distance. Analysis of the governing equations shows that there exists a ?most sensitive line? of initial vortex positions. When an initial state is on one side of the most sensitive line, the two vortices can obtain their global smallest distance and thus have a higher chance for merger. Conversely, when an initial state is on the other side relative to the most sensitive line, the two vortices can only obtain their local smallest distance. Consequently, they have a lower chance for merger. When an initial state is close to the most sensitive line, a very small initialization error can put this initial state on the wrong side of the most sensitive line, and the forecast evolution of the pair of vortices may be very different from the observed evolution. Numerical simulations that support these theoretical results are shown.
    publisherAmerican Meteorological Society
    titleVortex-Driven Sensitivity in Deformation Flow
    typeJournal Paper
    journal volume65
    journal issue12
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/2008JAS2745.1
    journal fristpage3819
    journal lastpage3839
    treeJournal of the Atmospheric Sciences:;2008:;Volume( 065 ):;issue: 012
    contenttypeFulltext
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