Research Article
A Two-Layer Hydrostatic-Reconstruction Method for High-Resolution Solving of the Two-Layer Shallow-Water Equations over Uneven Bed Topography
Figure 5
Computed (symbols) versus analytic (thick lines) layer surface levels (a) and discharges per unit width (b) at steady states, for the transcritical exchange flow over a hump test. The results for the parallel flow test case are shown in (c) and (d). The bed topography is shown at the bottom of each figure by the thin solid line and is plotted on the right -axis.