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    THE OCCURRENCE OF CRITICAL FLOW AND HYDRAULIC JUMPS IN A MULTI-LAYERED FLUID SYSTEM 

    Source: Journal of Meteorology:;1954:;volume( 011 ):;issue: 002:;page 139
    Author(s): Benton, George S.
    Publisher: American Meteorological Society
    Abstract: With use of the speed of long waves of infinitesimal amplitude as the criterion for critical flow, general expressions are obtained for critical conditions in a fluid system of n layers, where velocity as well as density ...
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    COMMENTS ON THE ANNUAL HEAT BALANCE OF THE NORTHERN HEMISPHERE 

    Source: Journal of Meteorology:;1954:;volume( 011 ):;issue: 006:;page 517
    Author(s): Benton, George S.
    Publisher: American Meteorological Society
    Abstract: No Abstract Available
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    Tidal Oscillations of an Enclosed Rotating Fluid 

    Source: Journal of Physical Oceanography:;1973:;Volume( 003 ):;issue: 001:;page 66
    Author(s): Hsueh, V.; Benton, George S.; Putland, G.
    Publisher: American Meteorological Society
    Abstract: Observations of surface waves in a tilted rotating circular basin of paraboloidal bottom reveal quantitatively the limitations of the predictability of tides by linear inviscid analyses. Through nonlinear interactions of ...
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    WATER-VAPOR TRANSFER OVER THE NORTH AMERICAN CONTINENT 

    Source: Journal of Meteorology:;1954:;volume( 011 ):;issue: 006:;page 462
    Author(s): Benton, George S.; Estoque, Mariano A.
    Publisher: American Meteorological Society
    Abstract: The transfer of water in vapor form by the atmosphere is presented for the calendar year 1949. Monthly and seasonal patterns of moisture flow are evaluated, and it is shown that there is a close relationship between these ...
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    SPECTRA OF LARGE-SCALE ATMOSPHERIC FLOW AT 300 MILLIBARS 

    Source: Journal of Meteorology:;1958:;volume( 015 ):;issue: 004:;page 404
    Author(s): Benton, George S.; Kahn, Arthur B.
    Publisher: American Meteorological Society
    Abstract: Data at 300 mb for January-February and July-August, 1949, are used to compute spectra of atmospheric turbulence as a function of wave number along various latitude circles. Power spectra are computed for the zonal and ...
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