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    Dynamic Systems at the Global Level 

    Source: Journal of Dynamic Systems, Measurement, and Control:;1991:;volume( 113 ):;issue: 001:;page 3
    Author(s): Harold Chestnut
    Publisher: The American Society of Mechanical Engineers (ASME)
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    Forum 

    Source: Journal of Dynamic Systems, Measurement, and Control:;1971:;volume( 093 ):;issue: 001:;page 3
    Author(s): Harold Chestnut
    Publisher: The American Society of Mechanical Engineers (ASME)
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    On the Representation of Isentropic Mixing in Ocean Circulation Models 

    Source: Journal of Physical Oceanography:;1971:;Volume( 001 ):;issue: 003:;page 233
    Author(s): Solomon, Harold
    Publisher: American Meteorological Society
    Abstract: tract
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    CAUSES CONTRIBUTORY TO THE ANNUAL VARIATION OF LATITUDE 

    Source: Monthly Weather Review:;1916:;Volume( 044 ):;issue: 006:;page 337
    Author(s): JEFFREYS, HAROLD
    Publisher: American Meteorological Society
    Abstract: No Abstract Available.
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    Discussion of “<i>Hyatt‐Regency Walkway Collapse: Design Alternates</i>” by George F. W. Hauck (May, 1983) 

    Source: Journal of Structural Engineering:;1984:;Volume ( 110 ):;issue: 004
    Author(s): Harold Engstrom
    Publisher: American Society of Civil Engineers
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    Amplification of Forced Rossby Waves in the Presence of a Nonlinear Critical Layer 

    Source: Journal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 012:;page 2012
    Author(s): Ritchie, Harold
    Publisher: American Meteorological Society
    Abstract: The nondivergent barotropic vorticity equation is integrated numerically in order to investigate a potential resonance mechanism for Rossby waves on a shear flow in the presence of a nonlinear critical layer. lie numerical ...
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    Application of a Semi-Lagrangian Integration Scheme to the Moisture Equation in a Regional Forecast Model 

    Source: Monthly Weather Review:;1985:;volume( 113 ):;issue: 004:;page 424
    Author(s): Ritchie, Harold
    Publisher: American Meteorological Society
    Abstract: Scale-dependent phase errors are characteristic of Eulerian advection schemes and can lead to significant erroneous dispersion, especially for features whose length scales are near the resolution limits of a numerical ...
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    Eliminating the Interpolation Associated with the Semi-Lagrangian Scheme 

    Source: Monthly Weather Review:;1986:;volume( 114 ):;issue: 001:;page 135
    Author(s): Ritchie, Harold
    Publisher: American Meteorological Society
    Abstract: There are several reasons why it is desirable to eliminate the interpolation associated with the conventional semi-Larangian scheme. Interpolation leads to smoothing and is also the most costly operation associated with ...
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    Semi-Lagrangian Advection on a Gaussian Grid 

    Source: Monthly Weather Review:;1987:;volume( 115 ):;issue: 002:;page 608
    Author(s): Ritchie, Harold
    Publisher: American Meteorological Society
    Abstract: The treatment of advection is related to the stability, accuracy and efficiency of models used in numerical weather prediction. In order to remain stable, conventional Eulerian advection schemes must respect a Courant-Fr ...
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    A Note on the Conservation of Potential Vorticity Across a Discontinuity in Shallow Water with Application to Theories of Equatorial Dynamics and Rossby Lee Waves 

    Source: Journal of Physical Oceanography:;1979:;Volume( 009 ):;issue: 005:;page 1032
    Author(s): Solomon, Harold
    Publisher: American Meteorological Society
    Abstract: It is shown that potential vorticity, as usually defined for slow motions in shallow water, is conserved across a discontinuity in bottom slope if the total depth is continuous, but not across a discontinuity in the depth ...
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