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    Three-Dimensional Mesoscale Dipole Frontal Collisions

    Source: Journal of Physical Oceanography:;2007:;Volume( 037 ):;issue: 009::page 2331
    Author:
    Dubosq, Sara
    ,
    Viúdez, Álvaro
    DOI: 10.1175/JPO3105.1
    Publisher: American Meteorological Society
    Abstract: Frontal collisions of mesoscale baroclinic dipoles are numerically investigated using a three-dimensional, Boussinesq, and f-plane numerical model that explicitly conserves potential vorticity on isopycnals. The initial conditions, obtained using the potential vorticity initialization approach, consist of twin baroclinic dipoles, balanced (void of waves) and static and inertially stable, moving in opposite directions. The dipoles may collide in a close-to-axial way (cyclone?anticyclone collisions) or nonaxially (cyclone?cyclone or anticyclone?anticyclone collisions). The results show that the interacting vortices may bounce back and interchange partners, may merge reaching a tripole state, or may squeeze between the outer vortices. The formation of a stable tripole from two colliding dipoles is possible but is dependent on diffusion effects. It is found that the nonaxial dipole collisions can be characterized by the interchange between the domain-averaged potential and kinetic energy. Dipole collisions in two-dimensional flow display also a variety of vortex interactions, qualitatively similar to the three-dimensional cases.
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      Three-Dimensional Mesoscale Dipole Frontal Collisions

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4226153
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    contributor authorDubosq, Sara
    contributor authorViúdez, Álvaro
    date accessioned2017-06-09T17:18:44Z
    date available2017-06-09T17:18:44Z
    date copyright2007/09/01
    date issued2007
    identifier issn0022-3670
    identifier otherams-82980.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4226153
    description abstractFrontal collisions of mesoscale baroclinic dipoles are numerically investigated using a three-dimensional, Boussinesq, and f-plane numerical model that explicitly conserves potential vorticity on isopycnals. The initial conditions, obtained using the potential vorticity initialization approach, consist of twin baroclinic dipoles, balanced (void of waves) and static and inertially stable, moving in opposite directions. The dipoles may collide in a close-to-axial way (cyclone?anticyclone collisions) or nonaxially (cyclone?cyclone or anticyclone?anticyclone collisions). The results show that the interacting vortices may bounce back and interchange partners, may merge reaching a tripole state, or may squeeze between the outer vortices. The formation of a stable tripole from two colliding dipoles is possible but is dependent on diffusion effects. It is found that the nonaxial dipole collisions can be characterized by the interchange between the domain-averaged potential and kinetic energy. Dipole collisions in two-dimensional flow display also a variety of vortex interactions, qualitatively similar to the three-dimensional cases.
    publisherAmerican Meteorological Society
    titleThree-Dimensional Mesoscale Dipole Frontal Collisions
    typeJournal Paper
    journal volume37
    journal issue9
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/JPO3105.1
    journal fristpage2331
    journal lastpage2344
    treeJournal of Physical Oceanography:;2007:;Volume( 037 ):;issue: 009
    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