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    ON PERMANENT PERTURBATIONS OF ZONAL ATMOSPHERIC MOTION, WITH APPLICATIONS TO LOW LATITUDES 

    Source: Journal of Meteorology:;1951:;volume( 008 ):;issue: 002:;page 84
    Author(s): Sherman, Leon
    Publisher: American Meteorological Society
    Abstract: If the pressure is eliminated from the vorticity equation, this vector equation and the continuity equation constitute a system of four, independent scalar equations in the four dependent variables, consisting of the ...
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    ON THE PROPAGATION OF ISOLINES 

    Source: Journal of Meteorology:;1953:;volume( 010 ):;issue: 003:;page 231
    Author(s): Sherman, Leon
    Publisher: American Meteorological Society
    Abstract: No Abstract Available
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    ESTIMATES OF THE VERTICAL VELOCITY BASED ON THE VORTICITY EQUATION 

    Source: Journal of Meteorology:;1953:;volume( 010 ):;issue: 005:;page 399
    Author(s): Sherman, Leon
    Publisher: American Meteorological Society
    Abstract: No Abstract Available
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    REPLY 

    Source: Journal of Meteorology:;1954:;volume( 011 ):;issue: 003:;page 258
    Author(s): Sherman, Leon
    Publisher: American Meteorological Society
    Abstract: No Abstract Available
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    A MECHANISM FOR PRODUCING CLOUD LINES 

    Source: Journal of Meteorology:;1952:;volume( 009 ):;issue: 002:;page 110
    Author(s): Sherman, Leon
    Publisher: American Meteorological Society
    Abstract: By consideration of the buoyancy effects associated with the release of latent heat, an hypothesis concerning a mechanism for the formation of cloud lines is set up. Adequate data for a quantitative check of this hypothesis ...
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    ON THE SCALAR-VORTICITY AND HORIZONTAL-DIVERGENCE EQUATIONS 

    Source: Journal of Meteorology:;1952:;volume( 009 ):;issue: 005:;page 359
    Author(s): Sherman, Leon
    Publisher: American Meteorological Society
    Abstract: It is desirable to treat the horizontal divergence as well as the vertical component of vorticity in reasoning about the wind field. One reason for this is that the vorticity is connected with the intensity of disturbances, ...
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    ON THE COMPUTATION OF HORIZONTAL DIVERGENCE 

    Source: Journal of Meteorology:;1955:;volume( 012 ):;issue: 001:;page 90
    Author(s): Sherman, Leon
    Publisher: American Meteorological Society
    Abstract: No Abstract Available
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    THE NEGLECT OF COMPRESSIBILITY IN THE FLOW OF GAS AT LOW SPEEDS 

    Source: Journal of Meteorology:;1949:;volume( 006 ):;issue: 004:;page 286
    Author(s): Sherman, Leon
    Publisher: American Meteorological Society
    Abstract: No Abstract Available
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    ON THE WIND ASYMMETRY OF HURRICANES 

    Source: Journal of Meteorology:;1956:;volume( 013 ):;issue: 005:;page 500
    Author(s): Sherman, Leon
    Publisher: American Meteorological Society
    Abstract: The difference in the wind speeds across hurricanes (from the ?dangerous? to the opposite semi-circle) is often greater than twice the speed of propagation of the storm. The traditional explanation of the speed asymmetry ...
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    REPLY 

    Source: Journal of Meteorology:;1957:;volume( 014 ):;issue: 004:;page 378
    Author(s): Sherman, Leon
    Publisher: American Meteorological Society
    Abstract: No Abstract Available.
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