A unified approach to energy conservation and potential vorticity dynamics for arbitrarily-structured C-grids
By Todd D. Ringler, John Thuburn, Joseph B. Klemp, William C. Skamarock. Journal of Computational Physics, 2010
307 citations recorded by the source corpus.
Subfields: Atmospheric Science, Earth-Surface Processes
View Paper: https://www.semanticscholar.org/paper/fb47485e1383592b2f246be083754dc1439d9c11
How researchers see this paper
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In Atmospheric Science
- J. Golaz
- Joseph B. Klemp
- V. Larson
- Elizabeth C. Hunke
- Stephen A. Klein
- M. Zelinka
- Sang Hun Park
- William C. Skamarock
In Earth-Surface Processes
Citations in the corpus
- A Multiscale Nonhydrostatic Atmospheric Model Using Centroidal Voronoi Tesselations and C-Grid Staggering (2012, methodology): “We employ a vector-invariant form of the horizontal momentum equation to avoid discretization difficulties on the unstructured mesh associated with the nonlinear momentum transport and to allow for potential vorticity conservation in the horizontal discretization (Ringler et al. 2010).”
- Can deep learning beat numerical weather prediction? (2021, background): “Simultaneously, remarkable progress has been achieved in designing discretization approaches which enable the grid-scale dynamics to follow the conservation laws of energy, enthrophy and mass [33,34] while also minimizing the need for numerical filters to suppress artificial numerical modes [35].”
- The DOE E3SM Coupled Model Version 1: Overview and Evaluation at Standard Resolution (2019, methodology): “MPAS-Ocean, based on the MPAS framework (Ringler et al., 2010), is the ocean component of E3SMv1 (Petersen et al. 2019).”
- Horizontal grids for global weather and climate prediction models: a review (2012, methodology): “…for example, by Nic̆ković (1994), Heikes and Randall (1995a,b), Giraldo (1997, 2000, 2005, 2006), Thuburn (1997), Stuhne and Peltier (1999), Ringler et al. (2000, 2010), Tomita et al. (2001), Ringler and Randall (2002a), Majewski et al. (2002), Randall et al. (2002), Tomita and Satoh…”
- A multi-resolution approach to global ocean modeling (2013, methodology): “In terms of energetics, the Coriolis force is computed so that it is energetically neutral (see Section 3 of Thuburn et al., 2009), and exchange of kinetic and potential energy is conservative (see (70) of Ringler et al., 2010).”