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    A Simplified Model of the Modified Hadley Circulation 

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 022:;page 3311
    Author(s): Schneider, Edwin K.
    Publisher: American Meteorological Society
    Abstract: A model is developed to find the low-latitude upper-tropospheric atmospheric circulation which would exist in the absence of transient eddies. The forcing in the model is zonally asymmetric to take into account the effect ...
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    Linear Diagnosis of Stationary Waves in a General Circulation Model 

    Source: Journal of the Atmospheric Sciences:;1989:;Volume( 047 ):;issue: 024:;page 2925
    Author(s): Schneider, Edwin K.
    Publisher: American Meteorological Society
    Abstract: A linear stationary wave model is used to diagnose the causes of stationary waves in integrations of a general circulation model (GCM) and to indicate the sources of differences between the stationary waves of separate ...
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    Trajectory Analysis of the Mechanism for Westward Propagation of Rossby Waves 

    Source: Journal of the Atmospheric Sciences:;2015:;Volume( 072 ):;issue: 005:;page 2178
    Author(s): Schneider, Edwin K.
    Publisher: American Meteorological Society
    Abstract: n analysis of Rossby wave dynamics in two and three dimensions is carried from the point of view of a reference frame propagating with the zonal phase speed of the wave. Since trajectories and streamlines coincide in this ...
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    On the Amplitudes Reached by Baroclinically Unstable Disturbances 

    Source: Journal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 010:;page 2142
    Author(s): Schneider, Edwin K.
    Publisher: American Meteorological Society
    Abstract: The maximum eddy energies reached by baroclinically unstable disturbances in some simplified numerical models (Gall, 1976b; Simmons and Hoskins, 1978) are compared to a scale-dependent measure of the energy available to ...
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    A Method for Direct Solution of a Steady Linearized Spectral General Circulation Model 

    Source: Monthly Weather Review:;1989:;volume( 117 ):;issue: 010:;page 2137
    Author(s): Schneider, Edwin K.
    Publisher: American Meteorological Society
    Abstract: A steady linearized version of a general circulation model (GCM) is a potentially useful tool for diagnosis and understanding of the time-mean solutions of the GCM. A method is developed for direct solution of the linearized ...
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    Response of the Annual and Zonal Mean Winds and Temperatures to Variations in the Heat and Momentum Sources 

    Source: Journal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 007:;page 1093
    Author(s): Schneider, Edwin K.
    Publisher: American Meteorological Society
    Abstract: The roles of eddy and zonal mean processes in producing the earth's annual-mean zonally-averaged tropospheric wind and temperature fields are investigated using a numerical zonally-averaged atmospheric model. First a ...
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    Some Minimization Calculations Concerning the Effect of Horizontal Eddy Momentum Fluxes on the Equilibrium Zonal Mean Motions 

    Source: Journal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 009:;page 1640
    Author(s): Schneider, Edwin K.
    Publisher: American Meteorological Society
    Abstract: A simplified linearized two-level zonally averaged atmospheric model and the calculus of variations are used to address the following problems: Assuming fixed thermal forcing except for the longwave, radiative response to ...
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    An Inconsistency in Vertical Discretization in Some Atmospheric Models 

    Source: Monthly Weather Review:;1987:;volume( 115 ):;issue: 009:;page 2166
    Author(s): Schneider, Edwin K.
    Publisher: American Meteorological Society
    Abstract: A simple example problem is constructed for which the continuous primitive equations are shown to have a solution. The model is then discretized in the vertical in a manner equivalent to that used in the NMC global spectral ...
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    Understanding Differences between the Equatorial Pacific as Simulated by Two Coupled GCMs 

    Source: Journal of Climate:;2002:;volume( 015 ):;issue: 005:;page 449
    Author(s): Schneider, Edwin K.
    Publisher: American Meteorological Society
    Abstract: Numerical experiments are performed to isolate the cause of differences between the simulations of SST in the low-latitude Pacific of two coupled atmosphere?ocean general circulation models, the Center for Ocean?Land?Atmosphere ...
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    Axially Symmetric Steady-State Models of the Basic State for Instability and Climate Studies. Part II. Nonlinear Calculations 

    Source: Journal of the Atmospheric Sciences:;1977:;Volume( 034 ):;issue: 002:;page 280
    Author(s): Schneider, Edwin K.
    Publisher: American Meteorological Society
    Abstract: The linearized model presented in Part I of this study (Schneider and Lindzen, 1977) is extended to include the nonlinear advections of angular momentum by the meridional circulation. A crude cumulus heating parameterization ...
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