A fully nonlinear Boussinesq model in generalized curvilinear coordinates

By Fengyan Shi, Robert A. Dalrymple, James T. Kirby, Q. Chen, A. Kennedy. 2001

115 citations recorded by the source corpus.

Subfields: Atmospheric Science, Earth-Surface Processes, Oceanography

View Paper: https://www.semanticscholar.org/paper/4d2d45a0f4bcb6b2c89a1148e18eb04956a6ef1c

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

In Earth-Surface Processes

In Oceanography

Citations in the corpus

A high-order adaptive time-stepping TVD solver for Boussinesq modeling of breaking waves and coastal inundation (2012, methodology): “At the same time, the curvilinear model developed by Shi et al. (2001) was implemented using a staggered grid for spatial differencing, and the resulting code was found to be less susceptible to the general grid noise problem.”
Dispersive tsunami waves in the ocean: Model equations and sensitivity to dispersion and Coriolis effects (2013, background): “…efficiency can be achieved by using nested grids (e.g., Ioualalen et al., 2007; Yamazaki et al., 2011; Son et al., 2011), unstructured or curvilinear grids (Shi et al., 2001) and parallelization of the computational algorithms (Sitanggang and Lynett, 2005; Pophet et al., 2011; Shi et al., 2012a).”
Boussinesq-type modelling using an unstructured finite element technique (2004, methodology): “Examples of the use of curvilinear mesh for solving the Boussinesq equations are given by Shi et al. (2001) and Li and Zhan (2001).”
A finite element method for the two‐dimensional extended Boussinesq equations (2002, background): “More recent work has investigated the use of boundary- tted grids which go some way to addressing this problem [17; 18]; however, the accuracy can be limited by the need for an orthogonal grid, and considerable work may be needed to generate such a grid for an arbitrary geometry.”
Oceanic propagation of a potential tsunami from the La Palma Island (2008, methodology): “In some respects these resemble the higher order spatial differences in FUNWAVE, but for the present model we must include temporal corrections as well.”