Efficient computation of surf zone waves using the nonlinear shallow water equations with non-hydrostatic pressure
By Marcel Zijlema, G. Stelling. 2008
257 citations recorded by the source corpus.
Subfields: Atmospheric Science, Earth-Surface Processes, Oceanography
View Paper: https://www.semanticscholar.org/paper/e8679f2bbd9f863ca9174cf7eb41749185073080
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
- Fengyan Shi
- Gangfeng Ma
- James T. Kirby
- Kwok Fai Cheung
- Y. Yamazaki
- Zygmunt Kowalik
- Stephan T. Grilli
- Jeffrey C. Harris
In Earth-Surface Processes
- Fengyan Shi
- James T. Kirby
- Gangfeng Ma
- Kwok Fai Cheung
- Y. Yamazaki
- Zygmunt Kowalik
- Stephan T. Grilli
- Jeffrey C. Harris
In Oceanography
- Fengyan Shi
- James T. Kirby
- Gangfeng Ma
- Kwok Fai Cheung
- Y. Yamazaki
- Zygmunt Kowalik
- Shijun Liao
- Stephan T. Grilli
Citations in the corpus
- Depth‐integrated, non‐hydrostatic model for wave breaking and run‐up (2009, background): “Overall, the upwind flux approximation (13a and 13b) and the second-order scheme (15a and 15b) in the present model provide the same or slightly better results compared with Stelling and Zijlema [12] and Walters [15].”
- Depth‐integrated, non‐hydrostatic model with grid nesting for tsunami generation, propagation, and run‐up (2010, unknown): “Zijlema and Stelling [22] and Yamazaki et al. [17], respectively, applied the momentum-conserved advection scheme in a two-layer and a depth-integrated non-hydrostatic model for breaking of dispersive waves with encouraging results.”
- Shock-capturing non-hydrostatic model for fully dispersive surface wave processes (2012, methodology): “Therefore, most existing models use a staggered grid in which the pressure is defined at the centers of computational cells and the velocities are defined at cell faces (Bradford, 2005).”