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    Instability of the Chaotic ENSO: The Growth-Phase Predictability Barrier 

    Source: Journal of the Atmospheric Sciences:;2001:;Volume( 058 ):;issue: 023:;page 3613
    Author(s): Samelson, Roger M.; Tziperman, Eli
    Publisher: American Meteorological Society
    Abstract: The local predictability of the El Niño?Southern Oscillation (ENSO) is examined by the analysis of the evolution of small disturbances to an unstable 4.3-yr ENSO cycle in the Cane?Zebiak model forced by perpetual July ...
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    Normal-Mode Analysis of a Baroclinic Wave-Mean Oscillation 

    Source: Journal of the Atmospheric Sciences:;2006:;Volume( 063 ):;issue: 011:;page 2795
    Author(s): Wolfe, Christopher L.; Samelson, Roger M.
    Publisher: American Meteorological Society
    Abstract: The stability of a time-periodic baroclinic wave-mean oscillation in a high-dimensional two-layer quasigeostrophic spectral model is examined by computing a full set of time-dependent normal modes (Floquet vectors) for the ...
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    Quasi-Geostrophic Topographically Generated Mean Flow over the Continental Margin 

    Source: Journal of Physical Oceanography:;1987:;Volume( 017 ):;issue: 011:;page 2043
    Author(s): Samelson, Roger M.; Allen, J. S.
    Publisher: American Meteorological Society
    Abstract: Observations of oppositely directed, monthly mean alongshore currents and wind stress over the continental margin off the Pacific coast of North America motivate the theoretical examination of mean flow generation by ...
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    The Duality between the Boussinesq and Non-Boussinesq Hydrostatic Equations of Motion 

    Source: Journal of Physical Oceanography:;2002:;Volume( 032 ):;issue: 007:;page 2194
    Author(s): de Szoeke, Roland A.; Samelson, Roger M.
    Publisher: American Meteorological Society
    Abstract: The hydrostatic equations of motion for ocean circulation, written in terms of pressure as the vertical coordinate, and without making the Boussinesq approximation in the continuity equation, correspond very closely with ...
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    Semigeostrophic Wind-Driven Thermocline Upwelling at a Coastal Boundary 

    Source: Journal of Physical Oceanography:;1988:;Volume( 018 ):;issue: 010:;page 1372
    Author(s): Samelson, Roger M.; de Szoeke, Roland A.
    Publisher: American Meteorological Society
    Abstract: We formulate analytically and solve numerically a semigeostrophic model for wind-driven thermocline upwelling at a coastal boundary. The model has a variable-density entraining mixed layer and two homogeneous interior ...
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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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    Singular Vectors and Time-Dependent Normal Modes of a Baroclinic Wave-Mean Oscillation 

    Source: Journal of the Atmospheric Sciences:;2008:;Volume( 065 ):;issue: 003:;page 875
    Author(s): Wolfe, Christopher L.; Samelson, Roger M.
    Publisher: American Meteorological Society
    Abstract: Linear disturbance growth is studied in a quasigeostrophic baroclinic channel model with several thousand degrees of freedom. Disturbances to an unstable, nonlinear wave-mean oscillation are analyzed, allowing the comparison ...
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    Coastal Atmospheric Circulation around an Idealized Cape during Wind-Driven Upwelling Studied from a Coupled Ocean–Atmosphere Model 

    Source: Monthly Weather Review:;2010:;volume( 139 ):;issue: 003:;page 809
    Author(s): Perlin, Natalie; Skyllingstad, Eric D.; Samelson, Roger M.
    Publisher: American Meteorological Society
    Abstract: The study analyzes atmospheric circulation around an idealized coastal cape during summertime upwelling-favorable wind conditions simulated by a mesoscale coupled ocean?atmosphere model. The domain resembles an eastern ...
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    Baroclinic Frontal Instabilities and Turbulent Mixing in the Surface Boundary Layer. Part II: Forced Simulations 

    Source: Journal of Physical Oceanography:;2017:;Volume( 047 ):;issue: 010:;page 2429
    Author(s): Skyllingstad, Eric D.;Duncombe, Jenessa;Samelson, Roger M.
    Publisher: American Meteorological Society
    Abstract: AbstractGeneration of ocean surface boundary layer turbulence and coherent roll structures is examined in the context of wind-driven and geostrophic shear associated with horizontal density gradients using a large-eddy ...
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    A Numerical Modeling Study of Warm Offshore Flow over Cool Water 

    Source: Monthly Weather Review:;2005:;volume( 133 ):;issue: 002:;page 345
    Author(s): Skyllingstad, Eric D.; Samelson, Roger M.; Mahrt, Larry; Barbour, Phil
    Publisher: American Meteorological Society
    Abstract: Numerical simulations of boundary layer evolution in offshore flow of warm air over cool water are conducted and compared with aircraft observations of mean and turbulent fields made at Duck, North Carolina. Two models are ...
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