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    The Integral Invariants of Two-Dimensional Inviscid Flow and Their Role in the Theory of Two-Dimensional Turbulence 

    Source: Journal of the Atmospheric Sciences:;1974:;Volume( 031 ):;issue: 005:;page 1453
    Author(s): Thompson, Philip Duncan
    Publisher: American Meteorological Society
    Abstract: It is shown that the invariance of the vorticity, kinetic energy and enstrophy integrals determines the form of the partial differential equation that governs the detailed evolution of two-dimensional nondivergent flows ...
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    A Simple Statistical Treatment of Highly Turbulent Couette Flow 

    Source: Journal of the Atmospheric Sciences:;1975:;Volume( 032 ):;issue: 003:;page 569
    Author(s): Thompson, Philip Duncan
    Publisher: American Meteorological Society
    Abstract: From the integral conditions for momentum and kinetic energy balance in the state of fully developed turbulence, it is found possible to estimate the bulk statistical properties of highly turbulent Couette flow as functions ...
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    How to Improve Accuracy by Combining Independent Forecasts 

    Source: Monthly Weather Review:;1977:;volume( 105 ):;issue: 002:;page 228
    Author(s): Thompson, Philip Duncan
    Publisher: American Meteorological Society
    Abstract: It is shown that the ensemble mean-square error of forecasts constructed from a particular linear combination of independent and imperfectly correlated predictions is less than that of any of the individual predictions. ...
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    THE PROPAGATION OF PERMANENT-TYPE WAVES IN HORIZONTAL FLOW 

    Source: Journal of Meteorology:;1948:;volume( 005 ):;issue: 004:;page 166
    Author(s): Thompson, Philip Duncan
    Publisher: American Meteorological Society
    Abstract: No Abstract Available
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    A THEORY OF LARGE-SCALE DISTURBANCES IN NON-GEOSTROPHIC FLOW 

    Source: Journal of Meteorology:;1956:;volume( 013 ):;issue: 003:;page 251
    Author(s): Thompson, Philip Duncan
    Publisher: American Meteorological Society
    Abstract: The primary aim of this article is to derive a complete system of modified hydrodynamical equations which govern a large class of ?meteorological? motions of the atmosphere, but which cannot generate solutions corresponding ...
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