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    A Terrain-Following Coordinate with Smoothed Coordinate Surfaces 

    Source: Monthly Weather Review:;2011:;volume( 139 ):;issue: 007:;page 2163
    Author(s): Klemp, J. B.
    Publisher: American Meteorological Society
    Abstract: n alternative form for a height-based terrain-following coordinate is presented here that progressively smoothes the coordinate surfaces with height to remove smaller scale (steeper) terrain structure from the surfaces. ...
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    Advection on Cut-Cell Grids for an Idealized Mountain of Constant Slope 

    Source: Monthly Weather Review:;2017:;volume( 145 ):;issue: 005:;page 1765
    Author(s): Steppeler, J.; Klemp, J. B.
    Publisher: American Meteorological Society
    Abstract: ut cells use regular or nearly regular polygonal cells to describe fields. For a given orography, some cells may be completely under the mountain, some completely above the mountain, and some are partially filled with air. ...
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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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    The Dynamics of Wave-Induced Downslope Winds 

    Source: Journal of the Atmospheric Sciences:;1975:;Volume( 032 ):;issue: 002:;page 320
    Author(s): Klemp, J. B.; Lilly, D. R.
    Publisher: American Meteorological Society
    Abstract: A theory for the dynamics of strong surface winds on the lee side of a large mountain range is derived and compared with observations. The strong winds observed near Boulder, Colo., are found to be surface manifestations ...
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    The Dependence of Numerically Simulated Convective Storms on Vertical Wind Shear and Buoyancy 

    Source: Monthly Weather Review:;1982:;volume( 110 ):;issue: 006:;page 504
    Author(s): Weisman, M. L.; Klemp, J. B.
    Publisher: American Meteorological Society
    Abstract: The effects of vertical wind shear and buoyancy on convective storm structure and evolution are investigated with the use of a three-dimensional numerical cloud model. By varying the magnitude of buoyant energy and ...
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    Numerical Simulation of Hydrostatic Mountain Waves 

    Source: Journal of the Atmospheric Sciences:;1978:;Volume( 035 ):;issue: 001:;page 78
    Author(s): Klemp, J. B.; Lilly, D. K.
    Publisher: American Meteorological Society
    Abstract: A numerical model is developed for simulating the flow of stably stratified nonrotating air over finite-amplitude, two-dimensional mountain ranges. Special attention is paid to accurate treatment of internal dissipation ...
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    Observed and Numerically Simulated Structure of a Mature Supercell Thunderstorm 

    Source: Journal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 008:;page 1558
    Author(s): Klemp, J. B.; Wilhelmson, R. B.; Ray, P. S.
    Publisher: American Meteorological Society
    Abstract: Through the interactive use of Doppler-radar analyses and a three-dimensional numerical storm simulation the detailed structure of a supercell, tornadic storm is analyzed. This storm, named the Del City storm, occurred in ...
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    Conservative Split-Explicit Time Integration Methods for the Compressible Nonhydrostatic Equations 

    Source: Monthly Weather Review:;2007:;volume( 135 ):;issue: 008:;page 2897
    Author(s): Klemp, J. B.; Skamarock, W. C.; Dudhia, J.
    Publisher: American Meteorological Society
    Abstract: Historically, time-split schemes for numerically integrating the nonhydrostatic compressible equations of motion have not formally conserved mass and other first-order flux quantities. In this paper, split-explicit integration ...
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    An Upper Gravity-Wave Absorbing Layer for NWP Applications 

    Source: Monthly Weather Review:;2008:;volume( 136 ):;issue: 010:;page 3987
    Author(s): Klemp, J. B.; Dudhia, J.; Hassiotis, A. D.
    Publisher: American Meteorological Society
    Abstract: Although the use of a damping layer near the top of a computational model domain has proven effective in absorbing upward-propagating gravity-wave energy in idealized simulations, this technique has been less successful ...
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    The Morphology of Several Tornadic Storms on 20 May 1977 

    Source: Journal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 008:;page 1643
    Author(s): Ray, P.S.; Johnson, B.C.; Johnson, K.W.; Bradberry, J.S.; Stephens, J.J.; Wagner, K.K; Wilhelmson, R.B.; Klemp, J.B.
    Publisher: American Meteorological Society
    Abstract: Sixteen tornadic storms occurred in the afternoon and evening hours of 20 May 1977 and the early morning hours of 21 May 1977. Three storms, two of them tornadic, have been selected for detailed study. One of the tornadic ...
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