A two‐time‐level semi‐Lagrangian global spectral model
暂无分享,去创建一个
[1] A. Robert. A Semi-Lagrangian and Semi-Implicit Numerical Integration Scheme for the Primitive Meteorological Equations , 1982 .
[2] J. R. Bates,et al. Improving the Estimate of the Departure Point Position in a Two-Time Level Semi-Lagrangian and Semi-Implicit Scheme , 1987 .
[3] Jean Côté,et al. A Two-Time-Level Semi-Lagrangian Semi-implicit Scheme for Spectral Models , 1988 .
[4] André Robert,et al. A stable numerical integration scheme for the primitive meteorological equations , 1981 .
[5] A. Staniforth,et al. The Operational CMC–MRB Global Environmental Multiscale (GEM) Model. Part I: Design Considerations and Formulation , 1998 .
[6] Jean-François Mahfouf,et al. The representation of soil moisture freezing and its impact on the stable boundary layer , 1999 .
[7] M. Tiedtke,et al. Representation of Clouds in Large-Scale Models , 1993 .
[8] Vladimir A Alexeev,et al. A Study of the Spurious Orographic Resonance in Semi-Implicit Semi-Lagrangian Models , 2000 .
[9] André Robert,et al. Spurious Resonant Response of Semi-Lagrangian Discretizations to Orographic Forcing: Diagnosis and Solution , 1994 .
[10] A. J. Simmons,et al. Stability of a Two-Time-Level Semi-Implicit Integration Scheme for Gravity Wave Motion , 1997 .
[11] J. Bates,et al. Forecast Experiments with a Global Finite-Difference Semi-Lagrangian Model , 1996 .
[12] Mats Hamrud,et al. Impact of model resolution and ensemble size on the performance of an Ensemble Prediction System , 1998 .
[13] Harold Ritchie,et al. Advantages of Spatial Averaging in Semi-implicit Semi-Lagrangian Schemes , 1992 .
[14] H. Ritchie,et al. A Comparison of Spatially Averaged Eulerian and Semi-Lagrangian Treatments of Mountains , 1996 .
[15] Shrinivas Moorthi,et al. NWP Experiments with a Gridpoint Semi-Lagrangian Semi-ImplicitGlobal Model at NCEP , 1997 .
[16] A. Simmons,et al. Implementation of the Semi-Lagrangian Method in a High-Resolution Version of the ECMWF Forecast Model , 1995 .
[17] François Lott,et al. A new subgrid‐scale orographic drag parametrization: Its formulation and testing , 1997 .
[18] Rodolfo Bermejo,et al. The Conversion of Semi-Lagrangian Advection Schemes to Quasi-Monotone Schemes , 1992 .
[19] N. Gustafsson,et al. A comparison of the HIRLAM gridpoint and spectral semi-Lagrangian models , 1996 .
[20] A. Staniforth,et al. The Operational CMC–MRB Global Environmental Multiscale (GEM) Model. Part II: Results , 1998 .
[21] Achi Brandt,et al. A global shallow‐water numerical model based on the semi‐lagrangian advection of potential vorticity , 1995 .
[22] Jan Erik Haugen,et al. A Two Time-Level, Three-Dimensional, Semi-Lagrangian, Semi-implicit, Limited-Area Gridpoint Model of the Primitive Equations. Part II: Extension to Hybrid Vertical Coordinates , 1993 .
[23] Adrian Simmons,et al. Use of Reduced Gaussian Grids in Spectral Models , 1991 .
[24] Philippe Courtier,et al. A pole problem in the reduced Gaussian grid , 1994 .
[25] Mariano Hortal,et al. The development and testing of a new two‐time‐level semi‐Lagrangian scheme (SETTLS) in the ECMWF forecast model , 2002 .
[26] J. Haugen,et al. A Two-Time-Level, Three-Dimensional Semi-Lagrangian, Semi-implicit, Limited-Area Gridpoint Model of the Primitive Equations , 1992 .
[27] Jean Côté,et al. A Generalized Family of Schemes that Eliminate the Spurious Resonant Response of Semi-Lagrangian Schemes to Orographic Forcing , 1995 .