Fig. 9From: A numerical shallow-water model for gravity currents for a wide range of density differencesNumerical results of h(x,t) for ρ c/ρ a=10. a BC model. b AB model with ε=1.0×10−10. In (b), ρ c/ρ a=10 is given when the basic equations (Eqs. (1) and (2)) are non-dimensionalized using Eqs. (4) and (5)Back to article page