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    HODOGRAPH ANALYSIS AS APPLIED TO THE OCCURRENCE OF CLEAR-AIR TURBULENCE 

    Source: Journal of Meteorology:;1959:;volume( 016 ):;issue: 005:;page 588
    Author(s): Schwerdtfeger, Werner; Radok, Uwe
    Publisher: American Meteorological Society
    Abstract: No Abstract Available.
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    Source: Journal of Meteorology:;1960:;volume( 017 ):;issue: 004:;page 477
    Author(s): Schwerdtfeger, Werner; Radok, Uwe
    Publisher: American Meteorological Society
    Abstract: No Abstract Available
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    THE SEMI-ANNUAL PRESSURE OSCILLATION, ITS CAUSE AND EFFECTS 

    Source: Journal of Meteorology:;1956:;volume( 013 ):;issue: 002:;page 217
    Author(s): Schwerdtfeger, Werner; Prohash, Frits
    Publisher: American Meteorological Society
    Abstract: No Abstract Available
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    Source: Monthly Weather Review:;1965:;volume( 093 ):;issue: 004:;page 226
    Author(s): SCHWERDTFEGER, WERNER; STROMMEN, NORTON D.
    Publisher: American Meteorological Society
    Abstract: No Abstract Available.
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    Source: Monthly Weather Review:;1966:;volume( 094 ):;issue: 005:;page 325
    Author(s): SCHWERDTFEGER, WERNER; STROMMEN, NORTON D.
    Publisher: American Meteorological Society
    Abstract: No Abstract Available.
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    The Zonal Flow of the Free Atmosphere Between 10N and 80S, in the South American Sector 

    Source: Journal of Applied Meteorology:;1964:;volume( 003 ):;issue: 006:;page 726
    Author(s): Schwerdtfeger, Werner; Martin, David W.
    Publisher: American Meteorological Society
    Abstract: Data from all available sources have been used to construct vertical cross sections of the seasonal mean flow of the atmosphere between 900 and 30 mb, over the western and southern part of South America. Monthly zonal wind ...
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    STRUCTURE OF A COLD FRONT NEAR THE CENTER OF AN EXTRATROPICAL DEPRESSION 

    Source: Monthly Weather Review:;1964:;volume( 092 ):;issue: 011:;page 523
    Author(s): SCHWERDTFEGER, WERNER; STROMMEN, NORTON D.
    Publisher: American Meteorological Society
    Abstract: Hourly aerological soundings released at Bedford, Mass. in April 1960, together with all available conventional synoptic observations, are used for a detailed analysis of a cold front south of the center of a northeastward-moving ...
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