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    The Shape of Large Tropospheric Clouds, or “Very Like a Whale” 

    Source: Bulletin of the American Meteorological Society:;1989:;volume( 070 ):;issue: 005:;page 468
    Author(s): Gifford, F. A.
    Publisher: American Meteorological Society
    Abstract: Lovejoy (1982) analyzed radar and satellite images of convective clouds and rainbands extending over an area range from 10 to 106 km2 and found the fractal cloud-perimeter dimension to equal 1.35, indicating the presence ...
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    A Similarity Theory of the Tropospheric Turbulence Energy Spectrum 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 008:;page 1370
    Author(s): Gifford, F. A.
    Publisher: American Meteorological Society
    Abstract: A three-range model is proposed for the energy spectrum of tropospheric turbulence in which the range-I spectrum is governed by the cascade of eddy enstrophy, that of range-II by the cascade of eddy kinetic energy, and ...
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    THE PROBLEM OF THE MARTIAN YELLOW CLOUDS 

    Source: Monthly Weather Review:;1963:;volume( 091 ):;issue: 010:;page 610
    Author(s): GIFFORD, F. A.
    Publisher: American Meteorological Society
    Abstract: No Abstract Available.
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    ADDENDUM TO “A STUDY OF MARTIAN YELLOW CLOUDS THAT DISPLAY MOVEMENT” 

    Source: Monthly Weather Review:;1964:;volume( 092 ):;issue: 011:;page 532
    Author(s): GIFFORD, F. A.
    Publisher: American Meteorological Society
    Abstract: No Abstract Available
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    The Rise of Strongly Radioactive Plumes 

    Source: Journal of Applied Meteorology:;1967:;volume( 006 ):;issue: 004:;page 644
    Author(s): Gifford, F. A.
    Publisher: American Meteorological Society
    Abstract: The presence of radioactive gases in a plume, such as could occur in the event of a nuclear reactor accident, leads to the addition of buoyancy to the plume at an approximately linear rate. Buoyancy might also be added to ...
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    Some Recent Long-Range Diffusion Observations 

    Source: Journal of Applied Meteorology:;1995:;volume( 034 ):;issue: 007:;page 1727
    Author(s): Gifford, F. A.
    Publisher: American Meteorological Society
    Abstract: Recent atmospheric cloud-spreading (relative diffusion) data from a variety of sources are combined to show that the horizontal spreading rate is approximately linear over a time range from 1 to 10 or more hours (20?200 ...
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    Tropospheric Relative Diffusion Observations 

    Source: Journal of Applied Meteorology:;1977:;volume( 016 ):;issue: 003:;page 311
    Author(s): Gifford, F. A.
    Publisher: American Meteorological Society
    Abstract: Data on relative on relative atmospheric diffusion, that is, the spreading by diffusion of puffs or particle pairs (e.g., of balloons) relative to their mutual center of mass, are reexamined. Richardson (1926) proposed his ...
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    The Vertical Variation of Atmospheric Eddy Energy Dissipation 

    Source: Journal of the Atmospheric Sciences:;1962:;Volume( 019 ):;issue: 002:;page 205
    Author(s): Gifford, F. A.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    Comments On Lateral Dispersion Coefficients as a Function of Averaging Time 

    Source: Journal of Applied Meteorology:;1981:;volume( 020 ):;issue: 002:;page 213
    Author(s): Gifford, F. A.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    WEATHER NOTE: OBSERVATION OF A HORIZONTAL CLOUDBOW 

    Source: Monthly Weather Review:;1964:;volume( 092 ):;issue: 002:;page 84
    Author(s): GIFFORD, F. A.
    Publisher: American Meteorological Society
    Abstract: No Abstract Available
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