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    The Baroclinic Instability of the Open Ocean 

    Source: Journal of Physical Oceanography:;1974:;Volume( 004 ):;issue: 003:;page 281
    Author(s): Robinson, A. R.; McWilliams, J. C.
    Publisher: American Meteorological Society
    Abstract: Baroclinic instability is examined in a two-layer, quasi-geostrophic model for linearized mesoscale waves (i.e., with periods of a few months and length scales near the internal deformation radius). The mid-ocean wave ...
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    A Coupled Air and Sea Model for the Tropical Pacific 

    Source: Journal of the Atmospheric Sciences:;1978:;Volume( 035 ):;issue: 006:;page 962
    Author(s): McWilliams, J. C.; Gent, P. R.
    Publisher: American Meteorological Society
    Abstract: Several sets of model equations are presented which represent coupled processes in the tropical atmosphere and ocean. The distribution of ocean surface temperature generates large-scale convective motions in the atmosphere. ...
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    Topographic Influences on Wind-Driven, Stratified Flow in a β-Plane Channel: An Idealized Model for the Antarctic Circumpolar Current 

    Source: Journal of Physical Oceanography:;1990:;Volume( 020 ):;issue: 003:;page 321
    Author(s): Treguier, A. M.; McWilliams, J. C.
    Publisher: American Meteorological Society
    Abstract: Topographic influences are examined in an eddy-resolving model of oceanic channel flow forced by steady zonal winds. With small explicit lateral friction, transient eddies generated by the baroclinic instability of the ...
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    Wave–Current Interaction: A Comparison of Radiation-Stress and Vortex-Force Representations 

    Source: Journal of Physical Oceanography:;2007:;Volume( 037 ):;issue: 005:;page 1122
    Author(s): Lane, E. M.; Restrepo, J. M.; McWilliams, J. C.
    Publisher: American Meteorological Society
    Abstract: The vortex-force representation of the wave-averaged effects on currents is compared to the radiation-stress representation in a scaling regime appropriate to coastal and shelf waters. Three-dimensional and vertically ...
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    Centrifugal Instability and Mixing in the California Undercurrent 

    Source: Journal of Physical Oceanography:;2015:;Volume( 045 ):;issue: 005:;page 1224
    Author(s): Dewar, W. K.; McWilliams, J. C.; Molemaker, M. J.
    Publisher: American Meteorological Society
    Abstract: regional numerical study of the California Current System near Monterey Bay, California, is conducted using both hydrostatic and nonhydrostatic models. Frequent sighting of strong anticyclones (Cuddies) have occurred in ...
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    Upper Ocean Thermal Response to Strong Autumnal Forcing of the Northeast Pacific 

    Source: Journal of Physical Oceanography:;1986:;Volume( 016 ):;issue: 009:;page 1524
    Author(s): Large, W. G.; McWilliams, J. C.; Niiler, P. P.
    Publisher: American Meteorological Society
    Abstract: CASID free-drifting thermistor chain buoys that utilized Service ARGOS positioning and data collection were deployed in the northeast Pacific Ocean in the vicinity of OWS-P in late autumn in both 1980 and 1981 as part of ...
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    Mesoscale to Submesoscale Transition in the California Current System. Part III: Energy Balance and Flux 

    Source: Journal of Physical Oceanography:;2008:;Volume( 038 ):;issue: 010:;page 2256
    Author(s): Capet, X.; McWilliams, J. C.; Molemaker, M. J.; Shchepetkin, A. F.
    Publisher: American Meteorological Society
    Abstract: This is the last of a suite of three papers about the transition that occurs in numerical simulations for an idealized equilibrium, subtropical, eastern-boundary upwelling current system similar to the California Current. ...
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    Properties of Steady Geostrophic Turbulence with Isopycnal Outcropping 

    Source: Journal of Physical Oceanography:;2011:;Volume( 042 ):;issue: 001:;page 18
    Author(s): Roullet, G.; McWilliams, J. C.; Capet, X.; Molemaker, M. J.
    Publisher: American Meteorological Society
    Abstract: igh-resolution simulations of ?-channel, zonal-jet, baroclinic turbulence with a three-dimensional quasigeostrophic (QG) model including surface potential vorticity (PV) are analyzed with emphasis on the competing role of ...
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    Dynamical Origin of Low-Frequency Variability in a Highly Nonlinear Midlatitude Coupled Model 

    Source: Journal of Climate:;2006:;volume( 019 ):;issue: 024:;page 6391
    Author(s): Kravtsov, S.; Berloff, P.; Dewar, W. K.; Ghil, M.; McWilliams, J. C.
    Publisher: American Meteorological Society
    Abstract: A novel mechanism of decadal midlatitude coupled variability, which crucially depends on the nonlinear dynamics of both the atmosphere and the ocean, is presented. The coupled model studied involves quasigeostrophic ...
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    Investigating 2D Modeling of Atmospheric Convection in the PBL 

    Source: Journal of the Atmospheric Sciences:;2004:;Volume( 061 ):;issue: 008:;page 889
    Author(s): Moeng, C-H.; McWilliams, J. C.; Rotunno, R.; Sullivan, P. P.; Weil, J.
    Publisher: American Meteorological Society
    Abstract: The performance of a two-dimensional (2D) numerical model in representing three-dimensional (3D) planetary boundary layer (PBL) convection is investigated by comparing the 2D model solution to that of a 3D large- eddy ...
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