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    GENERALIZED CRITERIA FOR DYNAMIC INSTABILITY 

    Source: Journal of Meteorology:;1950:;volume( 007 ):;issue: 004:;page 268
    Author(s): Godson, Warren L.
    Publisher: American Meteorological Society
    Abstract: The ?parcel? method of treating dynamic instability is extended to the case of an arbitrary flow pattern. The criteria for instability become relatively complex and depend on the three-dimensional gradients of temperature ...
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    SYNOPTIC SIGNIFICANCE OF DYNAMIC INSTABILITY 

    Source: Journal of Meteorology:;1950:;volume( 007 ):;issue: 005:;page 333
    Author(s): Godson, Warren L.
    Publisher: American Meteorological Society
    Abstract: The subsequent motion of a perturbed air-parcel is outlined, together with the criteria that determine the four fundamental types of dynamically stable and dynamically unstable motions. The specification of such motions ...
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    THE COMPUTATION OF INFRARED TRANSMISSION BY ATMOSPHERIC WATER VAPOR 

    Source: Journal of Meteorology:;1955:;volume( 012 ):;issue: 003:;page 272
    Author(s): Godson, Warren L.
    Publisher: American Meteorological Society
    Abstract: A basic problem in atmospheric radiation is the computation of flux transmission (hemispheric radiation) for a narrow interval of the water-vapor spectrum. Individual lines are spaced more or less at random and have widely ...
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    A NEW TENDENCY EQUATION AND ITS APPLICATION TO THE ANALYSIS OF SURFACE PRESSURE CHANGES 

    Source: Journal of Meteorology:;1948:;volume( 005 ):;issue: 005:;page 227
    Author(s): Godson, Warren L.
    Publisher: American Meteorological Society
    Abstract: From a consideration of temperature changes in isobaric surfaces a new pressure-tendency equation is derived which is applicable to mass changes of a layer or pressure changes at any level including the earth's surface. ...
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    THE ARCTIC STRATOSPHERIC JET STREAM DURING THE WINTER OF 1955–1956 

    Source: Journal of Meteorology:;1957:;volume( 014 ):;issue: 002:;page 126
    Author(s): Lee, Roy; Godson, Warren L.
    Publisher: American Meteorological Society
    Abstract: The existence of an Arctic stratospheric jet stream in winter, hitherto largely inferred from mean geostrophic wind sections, is considered on the basis of actual winds for the Canadian Arctic area during the winter of ...
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