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    The Slow Manifold of a Five-Mode Model 

    Source: Journal of the Atmospheric Sciences:;1994:;Volume( 051 ):;issue: 008:;page 1057
    Author(s): Boyd, John P.
    Publisher: American Meteorological Society
    Abstract: The slow manifold of an inviscid five-mode model introduced by Lorenz is investigated. When the influence of the gravity modes on the Rossby modes is neglected, the analytical solution given by Lorenz and Krishnamurthy is ...
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    The Energy Spectrum of Fronts: Time Evolution of Shocks in Burgers‚ Equation 

    Source: Journal of the Atmospheric Sciences:;1992:;Volume( 049 ):;issue: 002:;page 128
    Author(s): Boyd, John P.
    Publisher: American Meteorological Society
    Abstract: Andrews and Hoskins used semigeostrophic theory to argue that the energy spectrum of a front should decay like the ?8/3 power of the wavenumber. They note, however, that their inviscid analysis is restricted to the very ...
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    The Influence of Meridional Shear on Planetary Waves. Part 1: Nonsingular Wind Profiles 

    Source: Journal of the Atmospheric Sciences:;1982:;Volume( 039 ):;issue: 004:;page 756
    Author(s): Boyd, John P.
    Publisher: American Meteorological Society
    Abstract: Using a simple separable model in which the mean wind U(y) is assumed to be a function of latitude only, those effects of latitudinal shear which do not depend on the vanishing of U(y) are examined for planetary waves in ...
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    The Influence of Meridional Shear on Planetary Waves. Part 2: Critical Latitudes 

    Source: Journal of the Atmospheric Sciences:;1982:;Volume( 039 ):;issue: 004:;page 770
    Author(s): Boyd, John P.
    Publisher: American Meteorological Society
    Abstract: With the simplifying assumption that the mean zonal wind is a function of latitude only, numerical and analytical methods are applied to study the effects of critical latitudes (where the Doppler-shifted frequency is 0) ...
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    The Nonlinear Equatorial Kelvin Wave 

    Source: Journal of Physical Oceanography:;1980:;Volume( 010 ):;issue: 001:;page 1
    Author(s): Boyd, John P.
    Publisher: American Meteorological Society
    Abstract: Using the method of strained coordinates, a uniformly valid approximation to the nonlinear equatorial Kelvin wave is derived. It is shown that nonlinear effects are negligible for the Kelvin waves associated with the Gulf ...
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    Equatorial Solitary Waves. Part I: Rossby Solitons 

    Source: Journal of Physical Oceanography:;1980:;Volume( 010 ):;issue: 011:;page 1699
    Author(s): Boyd, John P.
    Publisher: American Meteorological Society
    Abstract: Using the method of multiple scales, I show that long, weakly nonlinear, equatorial Rossby waves are governed by either the Korteweg-deVries (KDV) equation (symmetric modes of odd mode number n) or the modified Korteweg-deVries ...
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    Limited-Area Fourier Spectral Models and Data Analysis Schemes: Windows, Fourier Extension, Davies Relaxation, and All That 

    Source: Monthly Weather Review:;2005:;volume( 133 ):;issue: 007:;page 2030
    Author(s): Boyd, John P.
    Publisher: American Meteorological Society
    Abstract: Regional spectral models have previously periodized and blended limited-area data through ad hoc low-order schemes justified by intuition and empiricism. By using infinitely differentiable ?window functions? or ?bells? ...
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    The Continuous Spectrum of Linear Couette Flow with the Beta Effect 

    Source: Journal of the Atmospheric Sciences:;1983:;Volume( 040 ):;issue: 009:;page 2304
    Author(s): Boyd, John P.
    Publisher: American Meteorological Society
    Abstract: The previously known analytic solution for the unbounded plane Couette flow [i.e., a mean flow U(y)=Sy, S constant] is extended by 1) inclusion of the beta effect, and 2) more general initial conditions. It is shown that ...
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    Barotropic Equatorial Waves: The Nonuniformity of the Equatorial Beta-Plane 

    Source: Journal of the Atmospheric Sciences:;1985:;Volume( 042 ):;issue: 018:;page 1965
    Author(s): Boyd, John P.
    Publisher: American Meteorological Society
    Abstract: Some equatorially trapped motions cannot be modeled by the equatorial beta-plane. Our proof is a counter-example: if the zonal wavenumber m is large, barotropic Rossby-Haurwitz waves decay with latitude outside a narrow ...
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    The Choice of Spectral Functions on a Sphere for Boundary and Eigenvalue Problems: A Comparison of Chebyshev, Fourier and Associated Legendre Expansions 

    Source: Monthly Weather Review:;1978:;volume( 106 ):;issue: 008:;page 1184
    Author(s): Boyd, John P.
    Publisher: American Meteorological Society
    Abstract: Modified Fourier series, as judged by criteria of accuracy, numerical efficiency and ease of programming, are the best choice of latitudinal expansion functions for general problems on the sphere. The pseudospectral and ...
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