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    A Note on the Barotropic Rossby Wave 

    Source: Journal of the Atmospheric Sciences:;1965:;Volume( 022 ):;issue: 003:;page 329
    Author(s): Fleagle, Robert G.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    The Case for a New NOAA Charter 

    Source: Bulletin of the American Meteorological Society:;1987:;volume( 068 ):;issue: 011:;page 1417
    Author(s): Fleagle, Robert G.
    Publisher: American Meteorological Society
    Abstract: The National Oceanic and Atmospheric Administration (NOAA) is not adequately equipped to meet the needs of the future for research, services, and information relating to the natural environment. A restructuring of NOAA is ...
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    THE FIELDS OF TEMPERATURE, PRESSURE, AND THREE-DIMENSIONAL MOTION IN SELECTED WEATHER SITUATIONS 

    Source: Journal of Meteorology:;1947:;volume( 004 ):;issue: 006:;page 165
    Author(s): Fleagle, Robert G.
    Publisher: American Meteorological Society
    Abstract: The fields of temperature, pressure, and three-dimensional motion are shown on horizontal charts and vertical cross sections for a period of anticyclogenesis above a polar anticyclone and for periods of cyclogenesis in ...
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    Reply 

    Source: Journal of the Atmospheric Sciences:;1977:;volume( 034 ):;issue: 005:;page 125
    Author(s): Fleagle, Robert G.
    Publisher: American Meteorological Society
    Abstract: tract
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    ADDITIONAL REMARKS 

    Source: Journal of Meteorology:;1954:;volume( 011 ):;issue: 006:;page 514
    Author(s): Fleagle, Robert G.
    Publisher: American Meteorological Society
    Abstract: No Abstract Available
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    COMMENTS ON "A STUDY OF VERTICAL VELOCITIES IN THE VICINITY OF JET STREAMS" 

    Source: Journal of Meteorology:;1954:;volume( 011 ):;issue: 006:;page 513
    Author(s): Fleagle, Robert G.
    Publisher: American Meteorological Society
    Abstract: No Abstract Available
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    RADIATION THEORY OF LOCAL TEMPERATURE DIFFERENCES 

    Source: Journal of Meteorology:;1950:;volume( 007 ):;issue: 002:;page 114
    Author(s): Fleagle, Robert G.
    Publisher: American Meteorological Society
    Abstract: It is shown that the lowest temperature to which a radiating surface may fall depends upon the thickness of the ground surface layer which undergoes temperature change, the conductivity of the layer, and the presence of ...
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    A THEORY OF AIR DRAINAGE 

    Source: Journal of Meteorology:;1950:;volume( 007 ):;issue: 003:;page 227
    Author(s): Fleagle, Robert G.
    Publisher: American Meteorological Society
    Abstract: The equation of motion is derived for a compressible fluid cooling at the bottom by contact with a radiating surface of uniform slope and large extent. During the early stages the drainage velocity is found to vary ...
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    ON THE MECHANISM OF LARGE-SCALE VERTICAL MOTION 

    Source: Journal of Meteorology:;1958:;volume( 015 ):;issue: 003:;page 249
    Author(s): Fleagle, Robert G.
    Publisher: American Meteorological Society
    Abstract: An equation is derived from the linearized equations of planetary aerodynamics which expresses the vertical component of velocity as a function of baroclinity, static stability, geostrophic vorticity, and geostrophic wind ...
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    QUANTITATIVE ANALYSIS OF FACTORS INFLUENCING PRESSURE CHANGE 

    Source: Journal of Meteorology:;1948:;volume( 005 ):;issue: 006:;page 281
    Author(s): Fleagle, Robert G.
    Publisher: American Meteorological Society
    Abstract: The contribution to density change made by local compression or expansion, advection, and vertical motion, and by horizontal mass divergence or convergence is determined for 132 cases chosen during a period of anticyclogenesis ...
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