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    Comments on “A Nonhydrostatic Version of the Penn State—NCAR Mesoscale Model: Validation Tests and Simulation of an Atlantic Cyclone and Cold Front" 

    Source: Monthly Weather Review:;1995:;volume( 123 ):;issue: 008:;page 2572
    Author(s): Steppeler, J.
    Publisher: American Meteorological Society
    Abstract: No abstract available
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    Quadratic Galerkin Finite Element Schemes for the Vertical Discretization of Numerical Forecast Models 

    Source: Monthly Weather Review:;1987:;volume( 115 ):;issue: 008:;page 1575
    Author(s): Steppeler, J.
    Publisher: American Meteorological Society
    Abstract: A finite element scheme with second-order basis functions is introduced for vertical discretization using a spectral model for horizontal discretization. The basis functions are required to be continuous, and no assumption ...
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    The Southern Oscillation as an Example of a Simple, Ordered Subsystem of a Complex Chaotic System 

    Source: Journal of Climate:;1997:;volume( 010 ):;issue: 003:;page 473
    Author(s): Steppeler, J.
    Publisher: American Meteorological Society
    Abstract: Complex chaotic systems are systems of high dimension and are unpredictable but often contain subsystems that are simple and predictable. The existence of such simple, ordered subsystems would indicate a predictability of ...
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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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    Third-Order Finite-Difference Schemes on Icosahedral-Type Grids on the Sphere 

    Source: Monthly Weather Review:;2008:;volume( 136 ):;issue: 007:;page 2683
    Author(s): Steppeler, J.; Rípodas, P.; Jonkheid, B.; Thomas, S.
    Publisher: American Meteorological Society
    Abstract: A practical method is proposed to achieve high-order finite-difference schemes on grids that are quasi-homogeneous on the sphere. A family of grids is used that are characterized by the parameter NP, which can take on ...
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    Challenges and Prospects for Numerical Techniques in Atmospheric Modeling 

    Source: Bulletin of the American Meteorological Society:;2023:;volume( 104 ):;issue: 002
    Author(s): Li, J.; Li, Y.; Steppeler, J.; Laurian, A.; Fang, F.; Knapp, D.
    Publisher: American Meteorological Society
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    Challenges and Prospects for Numerical Techniques in Atmospheric Modeling 

    Source: Bulletin of the American Meteorological Society:;2023:;volume( 104 ):;issue: 002:;page E449
    Author(s): Li, J.; Li, Y.; Steppeler, J.; Laurian, A.; Fang, F.; Knapp, D.
    Publisher: American Meteorological Society
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    o3o3: A Variant of Spectral Elements with a Regular Collocation Grid 

    Source: Monthly Weather Review:;2019:;volume 147:;issue 006:;page 2067
    Author(s): Steppeler, J.; Li, J.; Fang, F.; Zhu, J.; Ullrich, P. A.
    Publisher: American Meteorological Society
    Abstract: AbstractIn this study, an alternative local Galerkin method (LGM), the o3o3 scheme, is proposed. o3o3 is a variant or generalization of the third-order spectral element method (SEM3). It uses third-order piecewise polynomials ...
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    Prediction of Clouds and Rain Using a z-Coordinate Nonhydrostatic Model 

    Source: Monthly Weather Review:;2006:;volume( 134 ):;issue: 012:;page 3625
    Author(s): Steppeler, J.; Bitzer, H. W.; Janjic, Z.; Schättler, U.; Prohl, P.; Gjertsen, U.; Torrisi, L.; Parfinievicz, J.; Avgoustoglou, E.; Damrath, U.
    Publisher: American Meteorological Society
    Abstract: The most common option for numerical models of the atmosphere is to use model layers following the surface of the earth, using a terrain-following vertical coordinate. The present paper investigates the forecast of clouds ...
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