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    Wave-Permeable Lateral Boundary Conditions for Convective Cloud and Storm Simulations 

    Source: Journal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 006:;page 1313
    Author(s): Lilly, D. K.
    Publisher: American Meteorological Society
    Abstract: Linearized conditional instability theory is used to test the effects of lateral boundary conditions on convective elements. By this theory the outer environment of an amplifying convective element acts like an internal ...
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    Comments on “Case Studies of a Convective Plume and a Dust Devil” 

    Source: Journal of Applied Meteorology:;1971:;volume( 010 ):;issue: 003:;page 590
    Author(s): Lilly, D. K.
    Publisher: American Meteorological Society
    Abstract: tract
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    Stratified Turbulence and the Mesoscale Variability of the Atmosphere 

    Source: Journal of the Atmospheric Sciences:;1983:;Volume( 040 ):;issue: 003:;page 749
    Author(s): Lilly, D. K.
    Publisher: American Meteorological Society
    Abstract: An analysis is made of Gage's proposal that the horizontal energy spectrum at mesoscale wavelengths is produced by upscale energy transfer through quasi-two-dimensional turbulence. It is suggested that principal sources ...
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    A Note on Barotropic Instability and Predictability 

    Source: Journal of the Atmospheric Sciences:;1973:;Volume( 030 ):;issue: 001:;page 145
    Author(s): Lilly, D. K.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    A Severe Downslope Windstorm and Aircraft Turbulence Event Induced by a Mountain Wave 

    Source: Journal of the Atmospheric Sciences:;1978:;Volume( 035 ):;issue: 001:;page 59
    Author(s): Lilly, D. K.
    Publisher: American Meteorological Society
    Abstract: A detailed analysis is presented of the large-scale, mesoscale and turbulent-scale features of a major downslope windstorm event in central Colorado on 11 January 1972. The storm is found to be associated with a moderate ...
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    A PROPOSED STAGGERED-GRID SYSTEM FOR NUMERICAL INTEGRATION OF DYNAMIC EQUATIONS 

    Source: Monthly Weather Review:;1961:;volume( 089 ):;issue: 003:;page 59
    Author(s): LILLY, D. K.
    Publisher: American Meteorological Society
    Abstract: A system is proposed for grid allocation and differencing of apparently general applicability to purely marching-type systems of equations of fluid dynamics. The method is based on casting of the equations into the ...
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    THE DYNAMIC STRUCTURE OF LEE WAVE FLOW AS OBTAINED FROM BALLOON AND AIRPLANE OBSERVATIONS 

    Source: Monthly Weather Review:;1970:;volume( 098 ):;issue: 003:;page 220
    Author(s): VERGEINER, I.; LILLY, D. K.
    Publisher: American Meteorological Society
    Abstract: The lee flow disturbances produced by the Front Range of the Colorado Rockies have been quantitatively observed in a continuing program at the National Center for Atmospheric Research. The results of midtroposphere ...
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    The Carbonated-water Tornado Vortex 

    Source: Journal of the Atmospheric Sciences:;1963:;Volume( 020 ):;issue: 005:;page 468
    Author(s): Turner, J. S.; Lilly, D. K.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    Comments on “The Evolution and Stability of Finite-Amplitude Mountain Waves. Part II: Surface Wave Drag and Severe Downslope Windstorms” 

    Source: Journal of the Atmospheric Sciences:;1980:;Volume( 037 ):;issue: 009:;page 2119
    Author(s): Lilly, D. K.; Klemp, J. B.
    Publisher: American Meteorological Society
    Abstract: Not available
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    Observations of a Stationary Mountain Wave and its Associated Momentum Flux and Energy Dissipation 

    Source: Journal of the Atmospheric Sciences:;1973:;Volume( 030 ):;issue: 006:;page 1135
    Author(s): Lilly, D. K.; Kennedy, P. J.
    Publisher: American Meteorological Society
    Abstract: Analysis is presented of data obtained from instrumented aircraft flying in a mountain wave of moderate amplitude west of Denver, Colo., on 17 February 1970. Emphasis is placed on determination of the downward flux of ...
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