Conservative Split-Explicit Time Integration Methods for the Compressible Nonhydrostatic Equations
By Joseph B. Klemp, William C. Skamarock, Jimy Dudhia. 2007
302 citations recorded by the source corpus.
Subfields: Atmospheric Science, Geophysics
View Paper: https://www.semanticscholar.org/paper/149bcd6f751caba4ff0f853b0296d5bc9d5a2c34
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In Atmospheric Science
- Christiane Jablonowski
- Joseph B. Klemp
- David L. Williamson
- William C. Skamarock
- David M. Romps
- Sang Hun Park
- Jimy Dudhia
- Michael G. Duda
In Geophysics
- William C. Skamarock
- Joseph B. Klemp
- Z. Kuang
- David M. Romps
- Christiane Jablonowski
- David L. Williamson
- Sang Hun Park
- Michael G. Duda
Citations in the corpus
- A Description of the Advanced Research WRF Model Version 4 (2019, methodology): “The time-split integration for the flux-form equations is described and analyzed in Klemp et al. (2007).”
- Do Undiluted Convective Plumes Exist in the Upper Tropical Troposphere (2010, methodology): “Integration uses a split-time scheme whereby a large time step is advanced using thirdorder Runge–Kutta, and each Runge–Kutta step is subdivided into smaller steps for the integration of fast acoustic and gravity modes (Klemp et al. 2007).”
- Evaluation of Global Atmospheric Solvers Using Extensions of the Jablonowski and Williamson Baroclinic Wave Test Case (2013, background): “Thus, unlike the initial perturbation test such as Polvani et al. (2004), there is no significant sensitivity to different diffusion schemes.”
- A Description of the Advanced Research WRF Version 3 (2008, background): “A complete analysis of this filter can be found in Klemp et al. (2008).”
- A Multiscale Nonhydrostatic Atmospheric Model Using Centroidal Voronoi Tesselations and C-Grid Staggering (2012, methodology): “The fully compressible nonhydrostatic equations are solved using the time-split integration technique described in Klemp et al. (2007) for the height-coordinate equations.”
- Nonhydrostatic Atmospheric Models and Operational Development at JMA (2007, unknown): “(2005) Klemp et al. (2007) Skamarock and Klemp (2007)”
- The pros and cons of diffusion, filters and fixers in Atmospheric General Circulation Models (2011, background): “In the model WRF the dimensionless and positive coefficient ˇ is typically set to ˇ D 0:01 (Klemp et al. 2007).”
- A time-split nonhydrostatic atmospheric model for weather research and forecasting applications (2008, methodology): “The gravest gravity-wave mode is the external mode which propagates at speeds similar to the acoustic modes, hence handling these modes on the acoustic step is necessary [17].”