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    Theoretical Experiments on Cumulus Dynamics 

    Source: Journal of the Atmospheric Sciences:;1983:;Volume( 040 ):;issue: 005:;page 1241
    Author(s): Koenig, L. Randall; Murray, Francis W.
    Publisher: American Meteorological Society
    Abstract: The sensitivity of a two-dimensional cloud model to changes in microphysical characteristics was examined using two soundings. The dynamical evolution of clouds having relatively warm bases was controlled more by rapidity ...
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    Ice-Bearing Cumulus Cloud Evolution: Numerical Simulation and General Comparison Against Observations 

    Source: Journal of Applied Meteorology:;1976:;volume( 015 ):;issue: 007:;page 747
    Author(s): Koenig, L. Randall; Murray, Francis W.
    Publisher: American Meteorological Society
    Abstract: A two-dimensional (axisymmetric) numerical cloud model with parameterized microphysics for water drops and ice particles is described. The parameterized liquid-phase processes include condensation, evaporation, autoconversion ...
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    Numerical Simulation of an Industrial Cumulus and Comparison with Observations 

    Source: Journal of Applied Meteorology:;1978:;volume( 017 ):;issue: 005:;page 655
    Author(s): Murray, Francis W.; Koenig, L. Randall; Tag, Paul M.
    Publisher: American Meteorological Society
    Abstract: A two-dimensional field-of-flow numerical model of cloud development is used to study a cloud that formed over a refinery as a result of heat dissipated to the atmosphere. The observed vertical structure of the atmosphere ...
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    A Comparison of Several Forms of Eddy Viscosity Parameterization in a Two-Dimensional Cloud Model 

    Source: Journal of Applied Meteorology:;1979:;volume( 018 ):;issue: 011:;page 1429
    Author(s): Tag, Paul M.; Murray, Francis W.; Koenig, L. Randall
    Publisher: American Meteorological Society
    Abstract: A two-dimensional model is used to test the effects of using several forms of eddy viscosity parameterization to simulate subgrid-scale turbulence. A well-documented observation of a quasi-steady cumulus cloud which formed ...
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