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    A Forward-Backward Time Integration Scheme to Treat Internal Gravity Waves 

    Source: Monthly Weather Review:;1980:;volume( 108 ):;issue: 004:;page 402
    Author(s): Sun, W. Y.
    Publisher: American Meteorological Society
    Abstract: A forward time difference in the momentum equations and a backward time difference in the thermodynamic equation is conditionally stable according to von Neumann?s stability analysis of linearized anelastic equations. In ...
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    Boundary-Layer Forcing as a Possible Trigger to a Squall-Line Formation 

    Source: Journal of the Atmospheric Sciences:;1979:;Volume( 036 ):;issue: 002:;page 235
    Author(s): Sun, W-Y.; Ogura, Y.
    Publisher: American Meteorological Society
    Abstract: The study of the life history of the 8 June 1966 squall line by Ogura and Chen (1977) indicates that a well-defined narrow hand of horizontal convergence was present at low levels prior to the appearance of first radar ...
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    Convection in the Lower Atmosphere and its Effects 

    Source: Journal of the Atmospheric Sciences:;1976:;Volume( 033 ):;issue: 001:;page 21
    Author(s): Kuo, H. L.; Sun, W. Y.
    Publisher: American Meteorological Society
    Abstract: The development of convection in the lower atmosphere created by diurnal heating of the earth's surface is investigated by the use of a nonlinear numerical model. It is found that under the influence of the stable ...
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    An Intercomparison of Model-Predicted Wave Breaking for the 11 January 1972 Boulder Windstorm 

    Source: Monthly Weather Review:;2000:;volume( 128 ):;issue: 003:;page 901
    Author(s): Doyle, J. D.; Durran, D. R.; Chen, C.; Colle, B. A.; Georgelin, M.; Grubisic, V.; Hsu, W. R.; Huang, C. Y.; Landau, D.; Lin, Y. L.; Poulos, G. S.; Sun, W. Y.; Weber, D. B.; Wurtele, M. G.; Xue, M.
    Publisher: American Meteorological Society
    Abstract: Two-dimensional simulations of the 11 January 1972 Boulder, Colorado, windstorm, obtained from 11 diverse nonhydrostatic models, are intercompared with special emphasis on the turbulent breakdown of topographically forced ...
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