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    A Numerical Investigation of the Stability of Isolated Shallow Water Vortices 

    Source: Journal of Physical Oceanography:;2000:;Volume( 030 ):;issue: 010:;page 2562
    Author(s): Stegner, A.; Dritschel, D. G.
    Publisher: American Meteorological Society
    Abstract: Motivated by observational data and recent numerical simulations showing that ageostrophic effects may play an important role in the dynamics and transport of large-scale vortices in the atmosphere and the oceans, the ...
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    Hierarchies of Balance Conditions for the f-Plane Shallow-Water Equations 

    Source: Journal of the Atmospheric Sciences:;2001:;Volume( 058 ):;issue: 016:;page 2411
    Author(s): Mohebalhojeh, A. R.; Dritschel, D. G.
    Publisher: American Meteorological Society
    Abstract: For the f-plane shallow-water primitive equations (PEs), hierarchies of balance conditions relating the gravity manifold (divergence δ and ageostrophic vorticity ? = f? ? g?2h) to the Rossby manifold (linearized potential ...
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    Vortex Dipole Formation by Baroclinic Instability of Boundary Currents 

    Source: Journal of Physical Oceanography:;2007:;Volume( 037 ):;issue: 006:;page 1661
    Author(s): Chérubin, L.; Carton, X.; Dritschel, D. G.
    Publisher: American Meteorological Society
    Abstract: In situ data of the Mediterranean Water undercurrents and eddies south of Portugal indicate that the undercurrents have a tubelike structure in potential vorticity and that dipole formation can occur when the lower ...
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    Downward Wave Propagation on the Polar Vortex 

    Source: Journal of the Atmospheric Sciences:;2005:;Volume( 062 ):;issue: 009:;page 3382
    Author(s): Scott, R. K.; Dritschel, D. G.
    Publisher: American Meteorological Society
    Abstract: This paper considers the propagation of waves on the edge of a stratospheric polar vortex, represented by a three-dimensional patch of uniform potential vorticity in a compressible quasigeostrophic system. Waves are ...
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    Vortex–Vortex Interactions in the Winter Stratosphere 

    Source: Journal of the Atmospheric Sciences:;2006:;Volume( 063 ):;issue: 002:;page 726
    Author(s): Scott, R. K.; Dritschel, D. G.
    Publisher: American Meteorological Society
    Abstract: This paper examines the interaction of oppositely signed vortices in the compressible (non-Boussinesq) quasigeostrophic system, with a view to understanding vortex interactions in the polar winter stratosphere. A series ...
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    Multiple Jets as PV Staircases: The Phillips Effect and the Resilience of Eddy-Transport Barriers 

    Source: Journal of the Atmospheric Sciences:;2008:;Volume( 065 ):;issue: 003:;page 855
    Author(s): Dritschel, D. G.; McIntyre, M. E.
    Publisher: American Meteorological Society
    Abstract: A review is given that focuses on why the sideways mixing of potential vorticity (PV) across its background gradient tends to be inhomogeneous, arguably a reason why persistent jets are commonplace in planetary atmospheres ...
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    Enhancement of Rossby Wave Breaking by Steep Potential Vorticity Gradients in the Winter Stratosphere 

    Source: Journal of the Atmospheric Sciences:;2004:;Volume( 061 ):;issue: 008:;page 904
    Author(s): Scott, R. K.; Dritschel, D. G.; Polvani, L. M.; Waugh, D. W.
    Publisher: American Meteorological Society
    Abstract: This work investigates the extent to which potential vorticity gradients affect the vertical propagation of planetary-scale Rossby waves on the edge of a stratospheric polar vortex and their eventual nonlinear saturation ...
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