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    Multiple Fquilibria for Cross-Gyre Flow between Subpolar and Subtropical Gyres 

    Source: Journal of Physical Oceanography:;1993:;Volume( 023 ):;issue: 008:;page 1754
    Author(s): Schopp, Richard
    Publisher: American Meteorological Society
    Abstract: A simple Sverdrup-type two-layer model that allows the outcropping of isopycnals is forced by wind stress, is completed with a frictional western boundary layer, and is investigated along the zero wind-stress curl line ...
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    Spinup toward Communication between Large Oceanic Subpolar and Subtropical Gyres 

    Source: Journal of Physical Oceanography:;1988:;Volume( 018 ):;issue: 009:;page 1241
    Author(s): Schopp, Richard
    Publisher: American Meteorological Society
    Abstract: An interpretation in terms of planetary waves is proposed, which sheds light on the dynamics underlying the large-scale cross-gyre geostrophic flow recently developed in a two-layer ventilated thermocline model. The ...
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    A Ventilated Middepth Circulation Model for the Eastern North Atlantic 

    Source: Journal of Physical Oceanography:;1986:;Volume( 016 ):;issue: 002:;page 344
    Author(s): Schopp, Richard; Arhan, Michel
    Publisher: American Meteorological Society
    Abstract: A mechanism is proposed, based on the assumption of ventilation, to explain the middepth northward flow observed in the North Atlantic. The main feature of the solution is that the outcropping line of an intermediate layer ...
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    The Wind-driven Circulation: Quasi-geostrophic Simulations and Theory for Nonsymmetric Winds 

    Source: Journal of Physical Oceanography:;1991:;Volume( 021 ):;issue: 009:;page 1438
    Author(s): Rhines, Peter B.; Schopp, Richard
    Publisher: American Meteorological Society
    Abstract: Simulations of the wind-driven Ocean circulation, carded out with an eddy-resolving quasi-geostrophic numerical model, and symmetric, idealized wind forcing have a large-scale structure that is predicted wen by the steady ...
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    Three-Dimensional Dynamics of the Subsurface Countercurrents and Equatorial Thermostad. Part I: Formulation of the Problem and Generic Properties 

    Source: Journal of Physical Oceanography:;2003:;Volume( 033 ):;issue: 012:;page 2588
    Author(s): Hua, Bach Lien; Marin, Frédéric; Schopp, Richard
    Publisher: American Meteorological Society
    Abstract: A fully three-dimensional primitive equation simulation is performed to ?reunite? the local equatorial dynamics of the subsurface countercurrents (SCCs) and thermostad with the large-scale tropical ventilated ocean dynamics. ...
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    Three-Dimensional Dynamics of the Subsurface Countercurrents and Equatorial Thermostad. Part II: Influence of the Large-Scale Ventilation and of Equatorial Winds 

    Source: Journal of Physical Oceanography:;2003:;Volume( 033 ):;issue: 012:;page 2610
    Author(s): Marin, Frédéric; Schopp, Richard; Hua, Bach Lien
    Publisher: American Meteorological Society
    Abstract: Sensitivity tests are performed to assess the respective influences of the large-scale ventilation and of the near-equatorial winds on the dynamics of the the subsurface countercurrents (SCCs) and thermostad. They show ...
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    Comments on “A New Theory for the Generation of the Equatorial Subsurface Countercurrents” 

    Source: Journal of Physical Oceanography:;2005:;Volume( 035 ):;issue: 008:;page 1494
    Author(s): Marin, Frédéric; Hua, Bach Lien; Schopp, Richard
    Publisher: American Meteorological Society
    Abstract: From a numerical simulation of the Atlantic Ocean, Jochum and Malanotte-Rizzoli provide evidence that the equatorial subsurface countercurrents can be triggered by tropical instability waves through eddy?mean flow interactions ...
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    Tracer Stirring around a Meddy: The Formation of Layering 

    Source: Journal of Physical Oceanography:;2014:;Volume( 045 ):;issue: 002:;page 407
    Author(s): Meunier, Thomas; Ménesguen, Claire; Schopp, Richard; Le Gentil, Sylvie
    Publisher: American Meteorological Society
    Abstract: he dynamics of the formation of layering surrounding meddy-like vortex lenses is investigated using primitive equation (PE), quasigeostrophic (QG), and tracer advection models. Recent in situ data inside a meddy confirmed ...
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    Equatorial Zonal Jet Formation through the Barotropic Instability of Low-Frequency Mixed Rossby–Gravity Waves, Equilibration by Inertial Instability, and Transition to Superrotation 

    Source: Journal of the Atmospheric Sciences:;2009:;Volume( 066 ):;issue: 009:;page 2600
    Author(s): Fruman, Mark D.; Hua, Bach Lien; Schopp, Richard
    Publisher: American Meteorological Society
    Abstract: Depth-dependent barotropic instability of short mixed Rossby?gravity (MRG) waves is proposed as a mechanism for the formation of equatorial zonal jets. High-resolution primitive equation simulations show that a single MRG ...
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    An Exchange Window for the Injection of Antarctic Intermediate Water into the South Pacific 

    Source: Journal of Physical Oceanography:;2007:;Volume( 037 ):;issue: 001:;page 31
    Author(s): Iudicone, Daniele; Rodgers, Keith B.; Schopp, Richard; Madec, Gurvan
    Publisher: American Meteorological Society
    Abstract: Antarctic Intermediate Water (AAIW) occupies the intermediate horizon of most of the world oceans. Formed in the Southern Ocean, it is characterized by a relative salinity minimum. With a new, denser in situ National ...
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