TY - JOUR
T1 - A residual-based shock capturing scheme for the continuous/discontinuous spectral element solution of the 2D shallow water equations
AU - Marras, Simone
AU - Kopera, Michal A.
AU - Constantinescu, Emil M.
AU - Suckale, Jenny
AU - Giraldo, Francis X.
N1 - Publisher Copyright:
© 2018 Elsevier Ltd
PY - 2018/4
Y1 - 2018/4
N2 - The high-order numerical solution of the non-linear shallow water equations is susceptible to Gibbs oscillations in the proximity of strong gradients. In this paper, we tackle this issue by presenting a shock capturing model based on the numerical residual of the solution. Via numerical tests, we demonstrate that the model removes the spurious oscillations in the proximity of strong wave fronts while preserving their strength. Furthermore, for coarse grids, it prevents energy from building up at small wave-numbers. When applied to the continuity equation to stabilize the water surface, the addition of the shock capturing scheme does not affect mass conservation. We found that our model improves the continuous and discontinuous Galerkin solutions alike in the proximity of sharp fronts propagating on wet surfaces. In the presence of wet/dry interfaces, however, the model needs to be enhanced with the addition of an inundation scheme which, however, we do not address in this paper.
AB - The high-order numerical solution of the non-linear shallow water equations is susceptible to Gibbs oscillations in the proximity of strong gradients. In this paper, we tackle this issue by presenting a shock capturing model based on the numerical residual of the solution. Via numerical tests, we demonstrate that the model removes the spurious oscillations in the proximity of strong wave fronts while preserving their strength. Furthermore, for coarse grids, it prevents energy from building up at small wave-numbers. When applied to the continuity equation to stabilize the water surface, the addition of the shock capturing scheme does not affect mass conservation. We found that our model improves the continuous and discontinuous Galerkin solutions alike in the proximity of sharp fronts propagating on wet surfaces. In the presence of wet/dry interfaces, however, the model needs to be enhanced with the addition of an inundation scheme which, however, we do not address in this paper.
KW - De-aliasing
KW - Dynamic artificial diffusion
KW - Element-based Galerkin methods
KW - High-order methods
KW - Large Eddy Simulation
KW - Shallow water equations
KW - Unified continuous/discontinuous Galerkin
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U2 - 10.1016/j.advwatres.2018.02.003
DO - 10.1016/j.advwatres.2018.02.003
M3 - Article
AN - SCOPUS:85044459832
SN - 0309-1708
VL - 114
SP - 45
EP - 63
JO - Advances in Water Resources
JF - Advances in Water Resources
ER -