A Discontinuous Galerkin Transport Scheme on the Cubed Sphere
By Ramachandran D. Nair, Stephen J. Thomas, R. Loft. 2005
185 citations recorded by the source corpus.
Subfields: Computational Mechanics
View Paper: https://www.semanticscholar.org/paper/29dd0af59dd0d611815412ca5e7a511bb81f6dce
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Computational Mechanics
- David L. Williamson
- Shian‐Jiann Lin
- William M. Putman
- Ramachandran D. Nair
- R. Loft
- Stephen J. Thomas
- Jonathan A. Weyn
- R. Caruana
Citations in the corpus
- Improving Data‐Driven Global Weather Prediction Using Deep Convolutional Neural Networks on a Cubed Sphere (2020, background): “This projection has been shown to give more uniformly-sized grid cells than the alternative gnomomic equidistant projection and to also produce better solutions to finite-difference [34] and discontinuous Galerkin approximations [28] to partial differential”
- The Evolution of Dynamical Cores for Global Atmospheric Models(125th Anniversary Issue of the Meteorological Society of Japan) (2007, methodology): “Nair et al. (2005) developed a conservative transport scheme based on the discontinuous Galerkin method on the cubed sphere.”
- Finite-volume transport on various cubed-sphere grids (2007, background): “The vortices (simulated at diametrically opposite vertices on the cubed-sphere as in [30]) are well resolved and differences from the numerical solution by day 6 are on the order of ±1e 3.”
- Horizontal grids for global weather and climate prediction models: a review (2012, unknown): “…Taylor et al., 1997; Thomas and Loft, 2000, 2002, 2005; Giraldo et al., 2003; Fournier et al., 2004; Giraldo and Rosmond, 2004; Dennis et al., 2005; Nair et al., 2005a,b; Rossmanith, 2006; Putman and Lin, 2007; Wang et al., 2007; Chen and Xiao, 2008; Lauritzen and Nair, 2008; St-Cyr et al., 2008;…”
- A Discontinuous Galerkin Global Shallow Water Model (2005, methodology): “We consider the flux form shallow water equations in curvilinear coordinates as described in Sadourny (1972). The governing equations for an inviscid flow of a thin layer of fluid in 2D are the horizontal momentum and continuity equations for the height h.”