You signed in with another tab or window. Reload to refresh your session.You signed out in another tab or window. Reload to refresh your session.You switched accounts on another tab or window. Reload to refresh your session.Dismiss alert
The nonlinear shallow water solvers, in 1-D and 2-D, exhibit spurious flows when topography is spatially variable.
Gassner, Winters, & Kopriva (2016) and Wintermeyer et al. (2017) have shown that a discretization based on the split form of the shallow water equations is well-balanced (preserves lake-at-rest) and is entropy conservative, provided an appropriate Riemann flux is given. Additionally, they've shown that minimal modifications are needed to adjust a conservative form solver to obtain an equivalent implementation.
The text was updated successfully, but these errors were encountered:
The nonlinear shallow water solvers, in 1-D and 2-D, exhibit spurious flows when topography is spatially variable.
Gassner, Winters, & Kopriva (2016) and Wintermeyer et al. (2017) have shown that a discretization based on the split form of the shallow water equations is well-balanced (preserves lake-at-rest) and is entropy conservative, provided an appropriate Riemann flux is given. Additionally, they've shown that minimal modifications are needed to adjust a conservative form solver to obtain an equivalent implementation.
The text was updated successfully, but these errors were encountered: