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    Critical Layer Effects on Atmospheric Solitary and Cnoidal Waves 

    Source: Journal of the Atmospheric Sciences:;1991:;Volume( 048 ):;issue: 014:;page 1613
    Author(s): Skyllingstad, Eric D.
    Publisher: American Meteorological Society
    Abstract: The interactions of atmospheric cnoidal waves with a critical level are examined using a two-dimensional numerical model. A cnoidal wave system is generated by applying a bore initial condition to a shallow surface-based ...
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    The Role of Internal Gravity Waves in the Equatorial Current System 

    Source: Journal of Physical Oceanography:;1994:;Volume( 024 ):;issue: 010:;page 2093
    Author(s): Skyllingstad, Eric D.; Denbo, Donald W.
    Publisher: American Meteorological Society
    Abstract: Using a two-dimensional nonhydrostatic model, experiments were performed to investigate the formation and maintenance of internal waves in the equatorial Pacific Ocean. The simulations show that internal waves are generated ...
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    Large-Eddy Simulation of Moist Convection during a Cold Air Outbreak over the Gulf Stream 

    Source: Journal of the Atmospheric Sciences:;2009:;Volume( 066 ):;issue: 005:;page 1274
    Author(s): Skyllingstad, Eric D.; Edson, James B.
    Publisher: American Meteorological Society
    Abstract: Cold air outflow over the Gulf Stream is modeled using a cloud-resolving large-eddy simulation model with three classes of precipitation. Simulations are conducted in a quasi-Lagrangian framework using an idealized sounding ...
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    Investigation of Upstream Boundary Layer Influence on Mountain Wave Breaking and Lee Wave Rotors Using a Large-Eddy Simulation 

    Source: Journal of the Atmospheric Sciences:;2009:;Volume( 066 ):;issue: 010:;page 3147
    Author(s): Smith, Craig M.; Skyllingstad, Eric D.
    Publisher: American Meteorological Society
    Abstract: Interactions between a turbulent boundary layer and nonlinear mountain waves are explored using a large-eddy simulation model. Simulations of a self-induced critical layer, which develop a stagnation layer and a strong ...
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    Baroclinic Frontal Instabilities and Turbulent Mixing in the Surface Boundary Layer. Part I: Unforced Simulations 

    Source: Journal of Physical Oceanography:;2012:;Volume( 042 ):;issue: 010:;page 1701
    Author(s): Skyllingstad, Eric D.; Samelson, R. M.
    Publisher: American Meteorological Society
    Abstract: nteraction between mixed layer baroclinic eddies and small-scale turbulence is studied using a nonhydrostatic large-eddy simulation (LES) model. Free, unforced flow evolution is considered, for a standard initialization ...
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    Numerical Simulation of Katabatic Flow with Changing Slope Angle 

    Source: Monthly Weather Review:;2005:;volume( 133 ):;issue: 011:;page 3065
    Author(s): Smith, Craig M.; Skyllingstad, Eric D.
    Publisher: American Meteorological Society
    Abstract: A large eddy simulation (LES) model and the Advanced Regional Prediction System (ARPS) model, which does not resolve turbulent eddies, are used to study the effect of a slope angle decrease on the structure of katabatic ...
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    Cloud-Resolving Large-Eddy Simulation of Tropical Convective Development and Surface Fluxes 

    Source: Monthly Weather Review:;2015:;volume( 143 ):;issue: 007:;page 2441
    Author(s): Skyllingstad, Eric D.; de Szoeke, Simon P.
    Publisher: American Meteorological Society
    Abstract: loud-resolving large-eddy simulations (LES) on a 500 km ? 500 km periodic domain coupled to a thermodynamic ocean mixed layer are used to study the effect of large-scale moisture convergence M on the convective population ...
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    Large-Eddy Simulation of Flow over Two-Dimensional Obstacles: High Drag States and Mixing 

    Source: Journal of Physical Oceanography:;2004:;Volume( 034 ):;issue: 001:;page 94
    Author(s): Skyllingstad, Eric D.; Wijesekera, Hemantha W.
    Publisher: American Meteorological Society
    Abstract: A three-dimensional large-eddy simulation (LES) model was used to examine how stratified flow interacts with bottom obstacles in the coastal ocean. Bottom terrain representing a 2D ridge was modeled using a finite-volume ...
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    Effects of Inversion Height and Surface Heat Flux on Downslope Windstorms 

    Source: Monthly Weather Review:;2011:;volume( 139 ):;issue: 012:;page 3750
    Author(s): Smith, Craig M.; Skyllingstad, Eric D.
    Publisher: American Meteorological Society
    Abstract: imulations are presented focusing on the role of temperature inversions in controlling the formation and strength of downslope wind storms. Three mechanisms are examined depending on the relative height of the inversion ...
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    Instability Processes in Simulated Finite-Width Ocean Fronts 

    Source: Journal of Physical Oceanography:;2020:;volume( 50 ):;issue: 009:;page 2781
    Author(s): Skyllingstad, Eric D.;Samelson, Roger M.
    Publisher: American Meteorological Society
    Abstract: A simple, isolated front is modeled using a turbulence resolving, large-eddy simulation (LES) to examine the generation of instabilities and inertial oscillations by surface fluxes. Both surface cooling and surface wind ...
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