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    Convective Motion as Indicated by Visual Tracers 

    Source: Journal of Applied Meteorology:;1969:;volume( 008 ):;issue: 004:;page 506
    Author(s): Berry, Edwin X.
    Publisher: American Meteorological Society
    Abstract: Time-lapse photographs taken of a visual tracer laid in horizontal lines at several levels, one above the other, show convective motion of the air in a vertical plane. Through minor improvements in technique a three-dimensional ...
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    A Mathematical Framework for Cloud Models 

    Source: Journal of the Atmospheric Sciences:;1969:;Volume( 026 ):;issue: 001:;page 109
    Author(s): Berry, Edwin X.
    Publisher: American Meteorological Society
    Abstract: A mathematical framework is described which allows the logical joining of the processes of condensation, collection and advection, and also freezing and electrical effects in a cloud model.
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    Development and Use of an Airborne Air Marker for Atmospheric Research 

    Source: Journal of Applied Meteorology:;1969:;volume( 008 ):;issue: 004:;page 502
    Author(s): Nielsen, Klaus W.; Berry, Edwin X.
    Publisher: American Meteorological Society
    Abstract: Common motor oil is injected into the exhaust manifold of an aircraft where it is vaporized, and then mixes into the cold outside air to condense into a dense oil fog. This air marking technique has been used in atmospheric ...
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    An Analysis of Cloud Drop Growth by Collection: Part III. Accretion and Self-collection 

    Source: Journal of the Atmospheric Sciences:;1974:;Volume( 031 ):;issue: 008:;page 2118
    Author(s): Berry, Edwin X.; Reinhardt, Richard L.
    Publisher: American Meteorological Society
    Abstract: Accretion is shown to have a narrowing effect on the drop size distribution while the newly defined processes ?large hydrometeor self-collection, ? is shown to he responsible for the rapid growth of large hydrometeors and ...
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    An Analysis of Cloud Drop Growth by Collection: Part I. Double Distributions 

    Source: Journal of the Atmospheric Sciences:;1974:;Volume( 031 ):;issue: 007:;page 1814
    Author(s): Berry, Edwin X.; Reinhardt, Richard L.
    Publisher: American Meteorological Society
    Abstract: A new, highly accurate, yet fast method for the numerical solution of the stochastic collection equation is described. Basic size distribution parameters are defined that lay a basis for a parameterized description of ...
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    An Analysis of Cloud Drop Growth by Collection Part II. Single Initial Distributions 

    Source: Journal of the Atmospheric Sciences:;1974:;Volume( 031 ):;issue: 007:;page 1825
    Author(s): Berry, Edwin X.; Reinhardt, Richard L.
    Publisher: American Meteorological Society
    Abstract: The initial spreading of a cloud droplet distribution, its time of formation and placement of the second maximum, and the value of the minimum between the two maxima are systematically related to the mean mass and standard ...
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    An Analysis of Cloud Drop Growth by Collection: Part IV. A New Parameterization 

    Source: Journal of the Atmospheric Sciences:;1974:;Volume( 031 ):;issue: 008:;page 2127
    Author(s): Berry, Edwin X.; Reinhardt, Richard L.
    Publisher: American Meteorological Society
    Abstract: A new parameterization of cloud particle growth combines the effects of accretion and self-collection, and frees the large-hydrometeor water mass and spectral moments to grow independently. The large-hydrometeor water mass ...
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    Equations for Calculating the Terminal Velocities of Water Drops 

    Source: Journal of Applied Meteorology:;1974:;volume( 013 ):;issue: 001:;page 108
    Author(s): Berry, Edwin X.; Pranger, Maarten R.
    Publisher: American Meteorological Society
    Abstract: The experimental data of Gunn and Kinzer, Beard and Pruppacher, and Davies are used to curve-fit a polynomial for Re in terms of CdRe2. The resulting equations predict very accurately all known experimental data for drop ...
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